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Text
WELCOME TO BEAM
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field. EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toWELCOME TO BEAM
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field. EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields.CLOUD STRUCTURES
Clouds are the most mobile and changeable structure in the aspect of our live planet. Approaching the Earth it is impossible to look over their deversity, complexity and striking beauty. The following work is to describe some cloud formations over the ocean as well as present examples of some of the most frequently found cloud structures.CLOUD STRUCTURES
The small droplets reflect more lights (within the visible range) than large droplets, therefore the clouds of "Ship trails" structure have the higher brightness than the surrounding convective cells clouds. However within the infrared range they can be only badly recognized, because the cloud top height is low and accordingly warm.CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field.CLOUD STRUCTURES
The low pressure causes the air flow in the lee side of the barrier. When the air is humid, this leads to cloud formation. When the clouds come close to the air stream, which blows over the top, they will be swept away by its speed. The banner cloud stripes are formed. If a lone mountain defies to the wind as an only obstacle, the air willflow
CLOUD STRUCTURES
The Actinoform Structure (named after the greece actinos, a beam) may have two forms: round or oval cloud formation where there appear to be radial symmetry and sometimes even helical motion. These formations, when seen from high above, resemble veins of a leafe. In this case the dimension of the structure is from 80 to 400 km (seldom more).CLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de.ABOUT CALVALUS
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toWELCOME TO BEAM
EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de.ABOUT CALVALUS
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toWELCOME TO BEAM
EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields.CLOUD STRUCTURES
Clouds are the most mobile and changeable structure in the aspect of our live planet. Approaching the Earth it is impossible to look over their deversity, complexity and striking beauty. The following work is to describe some cloud formations over the ocean as well as present examples of some of the most frequently found cloud structures.CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The low pressure causes the air flow in the lee side of the barrier. When the air is humid, this leads to cloud formation. When the clouds come close to the air stream, which blows over the top, they will be swept away by its speed. The banner cloud stripes are formed. If a lone mountain defies to the wind as an only obstacle, the air willflow
CLOUD STRUCTURES
The small droplets reflect more lights (within the visible range) than large droplets, therefore the clouds of "Ship trails" structure have the higher brightness than the surrounding convective cells clouds. However within the infrared range they can be only badly recognized, because the cloud top height is low and accordingly warm.CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field.CLOUD STRUCTURES
The Actinoform Structure (named after the greece actinos, a beam) may have two forms: round or oval cloud formation where there appear to be radial symmetry and sometimes even helical motion. These formations, when seen from high above, resemble veins of a leafe. In this case the dimension of the structure is from 80 to 400 km (seldom more).CLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Dear valued customers and partners, o ur primary concern in this situation is the health and safety of our employees and their families. Since March 16th 2020, the majority of our employees ha ve been working in their home office s. In our office emergency staff ensures that all technical equipment is functioning and a contact person for all general matters is always on site. ABOUT CALVALUSSEE MORE ON BROCKMANN-CONSULT.DEWELCOME TO BEAM
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 stripsCLOUD STRUCTURES
"Peacock Feather" Cloud Structure (PFCS) The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”.CLOUD STRUCTURES
"Tropical Cyclone" (TCS) Tropical cyclones are regarded as a subtype of the "Mesoscale Convective System". They differ from the other cloudvortex forms by
EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for Global Earth Topography And Sea Surface Elevation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Dear valued customers and partners, o ur primary concern in this situation is the health and safety of our employees and their families. Since March 16th 2020, the majority of our employees ha ve been working in their home office s. In our office emergency staff ensures that all technical equipment is functioning and a contact person for all general matters is always on site. ABOUT CALVALUSSEE MORE ON BROCKMANN-CONSULT.DEWELCOME TO BEAM
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 stripsCLOUD STRUCTURES
"Peacock Feather" Cloud Structure (PFCS) The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”.CLOUD STRUCTURES
"Tropical Cyclone" (TCS) Tropical cyclones are regarded as a subtype of the "Mesoscale Convective System". They differ from the other cloudvortex forms by
EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for Global Earth Topography And Sea Surface Elevation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields.CLOUD STRUCTURES
"Washboard" Cloud Structure (WCS) The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape overand over again.
CLOUD STRUCTURES
"Convective Cells" "Ship Trails" Cloud Structure (STS) "Ship trails" cloud structure consists of stratocumulus (and at its edge of low cumulus) cloud lines.CLOUD STRUCTURES
An example of the "of the Morning Glory" Cloud Structure of 2007.02.08, orbit 25836: (from right to left) RGB image in the visual 412,691 Nm channel, Cloud topCLOUD STRUCTURES
"Orographic Clouds" (OC) Orographic clouds develop in response to the forced lifting of air by the earth's topography (mountains for example). Air passing over a mountain oscillates upCLOUD STRUCTURES
"Peacock Feather" Cloud Structure (PFCS) The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”.CLOUD STRUCTURES
"Convective Cells" 'Open Cell' Structure (OCS) & 'Enhanced Cumulus' Structure (ECS) An open cell consists of convective clouds, which top reaches only the lower layers of the troposphere.CLOUD STRUCTURES
'Kelvin-Helmholtz Instability' Cloud Structure (KHICS) The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speedand/or direction.
CLOUD STRUCTURES
"Convective Cells" "Actinoform" Structure(AFS) The Actinoform Structure (named after the greece actinos, a beam) may have two forms: . round or oval cloud formation where there appear to be radial symmetry and sometimes even helical motion. VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for Global Earth Topography And Sea Surface Elevation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt, BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt, ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields.CLOUD STRUCTURES
Clouds are the most mobile and changeable structure in the aspect of our live planet. Approaching the Earth it is impossible to look over their deversity, complexity and striking beauty. The following work is to describe some cloud formations over the ocean as well as present examples of some of the most frequently found cloud structures.CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonWELCOME TO BEAM
BEAM is an open-source toolbox and development platform for viewing, analysing and processing of remote sensing raster data. Originally developed to facilitate the utilisation of image data from Envisat's optical instruments, BEAM now supports a growing number of other raster data formats such as GeoTIFF and NetCDF as well as data formats of other EO sensors such as MODIS, AVHRR, AVNIR, PRISM SOFTWARE - BROCKMANN-CONSULT.DE Envisat Product Reader API for C (epr_api) comprises ANSI-C source code and API documentation. The API can be used to open Envisat MERIS and AATSR N1-files and to use the data in your C-programs. The latest source code can be obtained from the GitHub repository either as repository clone or as zip file. PyEPR is a python binding for theepr_api.
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field.CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 stripsCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt, BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to aCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt, ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields.CLOUD STRUCTURES
Clouds are the most mobile and changeable structure in the aspect of our live planet. Approaching the Earth it is impossible to look over their deversity, complexity and striking beauty. The following work is to describe some cloud formations over the ocean as well as present examples of some of the most frequently found cloud structures.CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonWELCOME TO BEAM
BEAM is an open-source toolbox and development platform for viewing, analysing and processing of remote sensing raster data. Originally developed to facilitate the utilisation of image data from Envisat's optical instruments, BEAM now supports a growing number of other raster data formats such as GeoTIFF and NetCDF as well as data formats of other EO sensors such as MODIS, AVHRR, AVNIR, PRISM SOFTWARE - BROCKMANN-CONSULT.DE Envisat Product Reader API for C (epr_api) comprises ANSI-C source code and API documentation. The API can be used to open Envisat MERIS and AATSR N1-files and to use the data in your C-programs. The latest source code can be obtained from the GitHub repository either as repository clone or as zip file. PyEPR is a python binding for theepr_api.
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field.CLOUD STRUCTURES
The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. These are round, oval or arc-like cloud forms or cloud series (with the cloud top height up to 3, rarely 3.5km), connected with each other and mixing with cloud lines often in the form ofsea-grass (cloud
CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 stripsCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
VISAT HELP - GETASSE30 ELEVATION MODEL GETASSE30 Elevation Model. GETASSE30 stands for G lobal E arth T opography A nd S ea S urface E levation at 30 arc second resolution. This elevation model is currently BEAM's default DEM and has kindly been provided to the BEAM development team by Marc Bouvet (marc.bouvet@esa.int) of ESA/ESRIN. This documentation is also by courtesy of Marc Bouvet. BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields. COPERNICUS SENTINEL-2 GLOBAL MOSAIC The Sentinel-2 Global Mosaic () service is a component of the Copernicus Land Monitoring Service providing composites from time-series of Sentinel-2 surface reflectance observations.S2GM comprises best representative pixels in three spatial resolutions and from different compositing periods ranging from one day to one year ona European scale.
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to SCIENTIFIC IMAGE PROCESSING TOOLBOX Scientific Image Processing Toolbox. SNAP stands for Sentinels Application Platform and is a common software architecture on which a collection of free open source toolboxes for the scientific exploitation of Earth Observation missions is available. SNAP is an ESA development, technically lead by Brockmann Consult, and availablethrough the ESA
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to a EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields. COPERNICUS SENTINEL-2 GLOBAL MOSAIC The Sentinel-2 Global Mosaic () service is a component of the Copernicus Land Monitoring Service providing composites from time-series of Sentinel-2 surface reflectance observations.S2GM comprises best representative pixels in three spatial resolutions and from different compositing periods ranging from one day to one year ona European scale.
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to SCIENTIFIC IMAGE PROCESSING TOOLBOX Scientific Image Processing Toolbox. SNAP stands for Sentinels Application Platform and is a common software architecture on which a collection of free open source toolboxes for the scientific exploitation of Earth Observation missions is available. SNAP is an ESA development, technically lead by Brockmann Consult, and availablethrough the ESA
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to a EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DECLOUD STRUCTURES
Clouds are the most mobile and changeable structure in the aspect of our live planet. Approaching the Earth it is impossible to look over their deversity, complexity and striking beauty. The following work is to describe some cloud formations over the ocean as well as present examples of some of the most frequently found cloud structures.CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field.WELCOME TO BEAM
BEAM is an open-source toolbox and development platform for viewing, analysing and processing of remote sensing raster data. Originally developed to facilitate the utilisation of image data from Envisat's optical instruments, BEAM now supports a growing number of other raster data formats such as GeoTIFF and NetCDF as well as data formats of other EO sensors such as MODIS, AVHRR, AVNIR, PRISMCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 stripsCLOUD STRUCTURES
"Peacock Feather" Cloud Structure (PFCS) The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. LA SOUFRIÈRE ERUPTION La Soufrière, a stratovolcano (1,220 m) on the Caribbean island of St Vincent, is one of the oldest volcanoes in the West Indies (about 60 million years old). On April 9 th, 2021 a massive explosive eruption occurred, with an ash plume reaching an altitude of about 6,100 mWEB SERVICES
This content is password protected. To view it please enter your password below: Password: GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt, BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields. COPERNICUS SENTINEL-2 GLOBAL MOSAIC The Sentinel-2 Global Mosaic () service is a component of the Copernicus Land Monitoring Service providing composites from time-series of Sentinel-2 surface reflectance observations.S2GM comprises best representative pixels in three spatial resolutions and from different compositing periods ranging from one day to one year ona European scale.
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to SCIENTIFIC IMAGE PROCESSING TOOLBOX Scientific Image Processing Toolbox. SNAP stands for Sentinels Application Platform and is a common software architecture on which a collection of free open source toolboxes for the scientific exploitation of Earth Observation missions is available. SNAP is an ESA development, technically lead by Brockmann Consult, and availablethrough the ESA
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to a EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300. Email: info@brockmann-consult.de. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields. COPERNICUS SENTINEL-2 GLOBAL MOSAIC The Sentinel-2 Global Mosaic () service is a component of the Copernicus Land Monitoring Service providing composites from time-series of Sentinel-2 surface reflectance observations.S2GM comprises best representative pixels in three spatial resolutions and from different compositing periods ranging from one day to one year ona European scale.
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down to SCIENTIFIC IMAGE PROCESSING TOOLBOX Scientific Image Processing Toolbox. SNAP stands for Sentinels Application Platform and is a common software architecture on which a collection of free open source toolboxes for the scientific exploitation of Earth Observation missions is available. SNAP is an ESA development, technically lead by Brockmann Consult, and availablethrough the ESA
CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
The sizes of the cyclone are from 500-700 km to 1200, rare 1500km. Its cloud top height reaches 12-15, to 16 km. The albedo is 0.8-1. Most tropical cyclones emerge above the sea surface within a zone, which lies between the southern and the northern latitudes of 30°, if the water temperature is min 26.5 °C up to a EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DECLOUD STRUCTURES
Clouds are the most mobile and changeable structure in the aspect of our live planet. Approaching the Earth it is impossible to look over their deversity, complexity and striking beauty. The following work is to describe some cloud formations over the ocean as well as present examples of some of the most frequently found cloud structures.CLOUD STRUCTURES
The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape over and over again. It is observed not often but regularly over an open ocean. The more than 50% of all observation cases lies over the Indian Ocean, in the south of equator from June to September (usually July - August - summer monsoon seasonCLOUD STRUCTURES
The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speed and/or direction. It can be assumed that due to the friction force between two air masses, which move with different speed, one (or several) irregularity in the form of penetration of a layer in theother one
CLOUD STRUCTURES
The cloud top height of an open cell is 1.5-2.5 km, (sometimes up to 3 km). The cloud top height of Enhanced Cumulus Clouds is up to 4-6 km, (rather often up to 7 km). Accordingly albedo increases from ~0.5 to ~0.8 (and even to 0.85). Space pictures often enable to see open and close cells sharing one and the same cloud field.WELCOME TO BEAM
BEAM is an open-source toolbox and development platform for viewing, analysing and processing of remote sensing raster data. Originally developed to facilitate the utilisation of image data from Envisat's optical instruments, BEAM now supports a growing number of other raster data formats such as GeoTIFF and NetCDF as well as data formats of other EO sensors such as MODIS, AVHRR, AVNIR, PRISMCLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 stripsCLOUD STRUCTURES
"Peacock Feather" Cloud Structure (PFCS) The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”. LA SOUFRIÈRE ERUPTION La Soufrière, a stratovolcano (1,220 m) on the Caribbean island of St Vincent, is one of the oldest volcanoes in the West Indies (about 60 million years old). On April 9 th, 2021 a massive explosive eruption occurred, with an ash plume reaching an altitude of about 6,100 mWEB SERVICES
This content is password protected. To view it please enter your password below: Password: GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt, BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Dear valued customers and partners, o ur primary concern in this situation is the health and safety of our employees and their families. Since March 16th 2020, the majority of our employees ha ve been working in their home office s. In our office emergency staff ensures that all technical equipment is functioning and a contact person for all general matters is always on site. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields. COPERNICUS SENTINEL-2 GLOBAL MOSAIC The Sentinel-2 Global Mosaic () service is a component of the Copernicus Land Monitoring Service providing composites from time-series of Sentinel-2 surface reflectance observations.S2GM comprises best representative pixels in three spatial resolutions and from different compositing periods ranging from one day to one year ona European scale.
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toCLOUD STRUCTURES
"Washboard" Cloud Structure (WCS) The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape overand over again.
CLOUD STRUCTURES
'Kelvin-Helmholtz Instability' Cloud Structure (KHICS) The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speedand/or direction.
CLOUD STRUCTURES
"Convective Cells" 'Open Cell' Structure (OCS) & 'Enhanced Cumulus' Structure (ECS) An open cell consists of convective clouds, which top reaches only the lower layers of the troposphere. EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
"Tropical Cyclone" (TCS) Tropical cyclones are regarded as a subtype of the "Mesoscale Convective System". They differ from the other cloudvortex forms by
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DE BROCKMANN CONSULTABOUT USAPPLICATIONSCAREERCONTACTIMPRINTSNAP Dear valued customers and partners, o ur primary concern in this situation is the health and safety of our employees and their families. Since March 16th 2020, the majority of our employees ha ve been working in their home office s. In our office emergency staff ensures that all technical equipment is functioning and a contact person for all general matters is always on site. ABOUT US – BROCKMANN CONSULT Our Vision. Successful projects and customer satisfaction can only be achieved by a motivated and highly skilled team. By keeping close contacts to universities and research institutes as well as participating in research projects, we maintain our state-of-the-art expertise in relevant scientific fields. COPERNICUS SENTINEL-2 GLOBAL MOSAIC The Sentinel-2 Global Mosaic () service is a component of the Copernicus Land Monitoring Service providing composites from time-series of Sentinel-2 surface reflectance observations.S2GM comprises best representative pixels in three spatial resolutions and from different compositing periods ranging from one day to one year ona European scale.
WATER QUALITY FROM SPACE The Colour of Water is determined by substances in the water, and measuring the water colour allows a retrieval of the water quality. Eutrophic waters appear green, while sediment loaded waters get a brown colour. Highly sensitive multispectral cameras, deployed on satellites, allow a quantification of such water constituents from space, at global scale and with a spatial resolution of down toCLOUD STRUCTURES
"Washboard" Cloud Structure (WCS) The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape overand over again.
CLOUD STRUCTURES
'Kelvin-Helmholtz Instability' Cloud Structure (KHICS) The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speedand/or direction.
CLOUD STRUCTURES
"Convective Cells" 'Open Cell' Structure (OCS) & 'Enhanced Cumulus' Structure (ECS) An open cell consists of convective clouds, which top reaches only the lower layers of the troposphere. EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 … evolution of the c2rcc neural network for sentinel 2 and 3 for the retrieval of ocean colour products in normal and extreme opticallycomplex waters
CLOUD STRUCTURES
"Tropical Cyclone" (TCS) Tropical cyclones are regarded as a subtype of the "Mesoscale Convective System". They differ from the other cloudvortex forms by
BEAM HELP - BEAM-DIMAP PRODUCT FORMATSEE MORE ON BROCKMANN-CONSULT.DECLOUD STRUCTURES
"Washboard" Cloud Structure (WCS) The "Washboard" Cloud Structure could be distinguished because it has been observed in its shape overand over again.
CLOUD STRUCTURES
An example of the "of the Morning Glory" Cloud Structure of 2007.02.08, orbit 25836: (from right to left) RGB image in the visual 412,691 Nm channel, Cloud topCLOUD STRUCTURES
'Kelvin-Helmholtz Instability' Cloud Structure (KHICS) The Kelvin-Helmholtz instability results from a turbulence of two air layers lying close to each other, which move with different speedand/or direction.
WELCOME TO BEAM
BEAM is an open-source toolbox and development platform for viewing, analysing and processing of remote sensing raster data. Originally developed to facilitate the utilisation of image data from Envisat's optical instruments, BEAM now supports a growing number of other raster data formats such as GeoTIFF and NetCDF as well as data formats of other EO sensors such as MODIS, AVHRR, AVNIR, PRISMCLOUD STRUCTURES
"Convective Cells" 'Open Cell' Structure (OCS) & 'Enhanced Cumulus' Structure (ECS) An open cell consists of convective clouds, which top reaches only the lower layers of the troposphere.CLOUD STRUCTURES
"Peacock Feather" Cloud Structure (PFCS) The clouds of this structure often look from above like the parts of peacock’s feather or also like cacti of the kind “Opuntia ovata”.CLOUD STRUCTURES
"Gravity Wave" Cloud Structure (GWCS) The gravity wave clouds above the water surface are not often observed. In contrast to much more frequently observing gravity wave clouds over the land, which normally above the lee side of mountains form and consist of long but not wide series, the gravity waves clouds above sea can have many hundreds kilometres long, but rarely more than 5-15 strips LA SOUFRIÈRE ERUPTION La Soufrière, a stratovolcano (1,220 m) on the Caribbean island of St Vincent, is one of the oldest volcanoes in the West Indies (about 60million years old).
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This content is password protected. To view it please enter your password below: Password: GUIDE TO TERRAVIVA! LAND COVER MAP Grassland: Lands with herbaceous types of cover. Tree and shrub cover is less than 10%. Permanent Wetland: Lands with a permanent mixture of water and herbaceous or woody vegetation that cover extensive areas. The vegetation can be present in salt,_ _
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REMOTE IS GETTING CLOSER COVID-19 INFORMATION Dear valued customers and partners, our primary concern in this situation is the health and safety of our employees and their families. Since March 16th 2020, the majority of our employees have been working in their home offices. In our office emergency staff ensures that all technical equipment is functioning and a contact person for all general matters is always on site. Home office has long been part of our daily work routine, and so our business continues to run almost without restriction. Perhaps you cannot reach a specific employee on the phone at the usual times. Therefore, please use email as a preferred communication medium. In any case you can also reach us as follows: Tel.: +49 40 69 63 89 – 300 Email: info@brockmann-consult.de TURNING DATA INTO KNOWLEDGE. The rapidly increasing amount of environmental data has dramatically changed the view of our planet – and continues to do so with the onset of a new generation of satellites, drones, and citizen science. We enable our customers to benefit from this new perspective. _CARSTEN BROCKMANN – Managing Director_GET IN TOUCH.
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Brockmann Consult takes pride in supporting top-tier institutions like ESA, EUMETSAT, and the European Commission as well as numerous smaller customers to reach their ambitious objectives since 1999. If it is about Earth Observation data – we will find a solution! ENVIRONMENTAL INFORMATICS We offer tailor-made software that effectively meets the requirements of our customers – regardless if it is just some lines of source code solving a very specific use case or a full-fledged software like our expert application SNAP,
the Sentinel Application Platform, for the exploitation of Earth Observation products from many different sensors. Our solutions enable experts as well as end users to make the most of the available EarthObservation data.
GEOINFORMATION SERVICES We turn the vast amount of Earth Observation data that is continuously produced by a growing fleet of satellites into valuable information on our environment and make it usable for public authorities, businesses, and the public. Our broad expertise allows us to offer the full range of services, marine and land applications with local, regional, andglobal scopes.
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