G. Heygster | University of Bremen (original) (raw)

Papers by G. Heygster

Research paper thumbnail of Atmospheric and Surface Processes, and Feedback Mechanisms Determining Arctic Amplification: A Review of First Results and Prospects of the (AC)3 Project

Bulletin of the American Meteorological Society

Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To contribute to t... more Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To contribute to this debate, the (AC)3 project has been established in 2016 (http://www.ac3-tr.de/). It comprises modeling and data analysis efforts as well as observational elements. The project has assembled a wealth of ground-based, airborne, ship-borne, and satellite data of physical, chemical, and meteorological properties of the Arctic atmosphere, cryosphere, and upper ocean that are available for the Arctic climate research community. Short-term changes and indications of long-term trends in Arctic climate parameters have been detected using existing and new data. For example, a distinct atmospheric moistening, an increase of regional storm activities, an amplified winter warming in the Svalbard and North Pole regions, and a decrease of sea ice thickness in the Fram Strait and of snow depth on sea ice have been identified. A positive trend of tropospheric bromine monoxide (BrO) column densities du...

Research paper thumbnail of сравнительный анализ трёх моделей интертипных отношений в соционе

Соционика, ментология и психология личности, 2018

Research paper thumbnail of ESA Sea Ice Climate Change Initiative (Sea_Ice_cci): Sea Ice Concentration Climate Data Record from the AMSR-E and AMSR-2 instruments at 50 km grid spacing, version 2.0

Research paper thumbnail of RESOURCE: an International Initiative for Radio Sciences Research on Antarctic Atmosphere

Research paper thumbnail of Image restoration for SAM using computed optical transfer functions

Optik, 1994

A theory for surface structure imaging is presented, which allows the computation of optical tran... more A theory for surface structure imaging is presented, which allows the computation of optical transfer functions (OTF) of the scanning acoustic microscope (SAM). The model describes the monitor image in terms of the reflectivity of the specimen, thus including the influence of the confocal lens system and subsequent signal processing. Amplitude and phase contrast imaging in SAM are defined, and the corresponding OTF computed for different focus positions are shown to be in good agreement with measurements. Based on the theoretical OTF, an image restoration scheme for phase contrast imaging is developed. Combining images of a focal series, the imaging properties of SAM for phase contrast can be improved

Research paper thumbnail of Thickness of thin sea ice retrieved from SMOS and SMAP

2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS), 2016

Sea ice is an important quantity for the radiation budget of the Earth's climate system. In t... more Sea ice is an important quantity for the radiation budget of the Earth's climate system. In this paper we present a comparison of SMAP and SMOS measured brightness temperatures and translate a validated retrieval algorithm for the thickness of thin sea ice from SMOS to SMAP radiometer observations. For October to December all observations of SMAP in forward and backward direction are compared as daily averages and found with low RMSD of 2.25K and 2.42K in TB,v and TB,h, respectively. The mean of forward and backward observations from SMAP are mapped to SMOS equivalent brightness temperatures using a linear regression. SMAP was found to yield lower brightness temperatures compared to SMOS by about 5K in both polarizations while difference decreases with increasing brightness temperatures. An existing ice thickness retrieval for SMOS using averaged brightness temperatures in the incidence angles range of 40° to 50° is transferred to SMAP using another linear regression. Ice thickn...

Research paper thumbnail of Inter-comparison and evaluation of sea ice algorithms: towards further identification of challenges and optimal approach using passive microwave observations

Research paper thumbnail of Intertidal Topographic Maps and Morphological Changes in the German Wadden Sea between 1996–1999 and 2006–2009 from the Waterline Method and SAR Images

IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 2014

ABSTRACT The Dutch, German, and Danish Wadden Sea is one of the largest tidal flats in the world ... more ABSTRACT The Dutch, German, and Danish Wadden Sea is one of the largest tidal flats in the world which has been left in a nearly natural state. Several studies generated the topography of this valuable area, but presented only single maps, which covered partial regions of the Wadden Sea. The objectives of this paper are 1) to use the waterline method to analyze SAR images in order to generate annual topographic maps of the northern parts of the German Wadden Sea for the years 1996-1999 and 2006-2009 and 2) to quantitatively estimate and monitor the development of the tidal flats. The waterlines are detected by a wavelet-based edge detection algorithm, geocoded in Gauss-Krueger coordinates, assigned with water level information, and interpolated into topographic maps. Our results show the development of the tidal flats over the 8 years and illustrate three of the most changing regions: Tertiussand, Gelbsand, and Medemsand. Their area, shape, and sediment volume have changed significantly due to the tide, wave, wind, and river discharge influences. The waterline method is an efficient and economical way to monitor large tidal flat areas, which allows an estimation of long-term morphological development. One potential application is to assimilate the results into morphodynamic models in order to give finer morphological predictions.

Research paper thumbnail of Retrieval of total water vapor in polar regions using SSM/T2 channels

IGARSS'97. 1997 IEEE International Geoscience and Remote Sensing Symposium Proceedings. Remote Sensing - A Scientific Vision for Sustainable Development, 1997

ABSTRACT A method to retrieve the total water vapor in the cloudless atmosphere using SSM/T2 chan... more ABSTRACT A method to retrieve the total water vapor in the cloudless atmosphere using SSM/T2 channels is proposed based on a unique property of three contiguous channels situated on the flank of the water vapor absorption line at 183.31 GHz. One of its advantages is its independence to the surface emission, which is the main disturbing factor in retrieving atmospheric parameters from passive satellite measurements. Due to the high sensitivity of the SSM/T2 channels to water vapor, this method is suitable to the total water vapor retrieval for dry polar atmospheres. An algorithm is constructed for austral winter cases through model simulation using radiosonde profiles

Research paper thumbnail of New approach for radiative transfer in sea ice and its application for sea ice satellite remote sensing

ABSTRACT In this paper we present the newly developed analytical description of the radiative tra... more ABSTRACT In this paper we present the newly developed analytical description of the radiative transfer in the sea ice in visible and near IR region and the idea and first results of the retrieval of the melt pond fractions from data of a satellite spectral sensor. This retrieval is based on the analytical description of the optical properties of sea ice as a scattering medium.

Research paper thumbnail of Response of passive microwave sea ice concentration algorithms to thin ice

2014 IEEE Geoscience and Remote Sensing Symposium, 2014

The influence of sea ice thickness brightness temperatures and ice concentrations retrieved from ... more The influence of sea ice thickness brightness temperatures and ice concentrations retrieved from passive microwave observations is quantified, using horizontally homogeneous sea ice thickness retrievals from ESA's SMOS sensor observations at high incidence angles. Brightness temperatures are influenced by thickness below 18 cm (89GHz) and 50 cm (1.4 GHz). Ice concentration retrievals reduced by ice thickness below 0.17 m and 0.33 m, with higher frequency algorithms being less influenced.

Research paper thumbnail of Exploring Arctic Transpolar Drift During Dramatic Sea Ice Retreat

Eos, Transactions American Geophysical Union, 2008

Research paper thumbnail of AMS Journals Online - POLAR PROGRAM: Integrated

Research paper thumbnail of Comparison of Tropospheric Water Vapour over Antarctica Derived from AMSU-B Data, Ground-Based GPS Data and the NCEP/NCAR Reanalysis

Journal of the Meteorological Society of Japan, 2004

Research paper thumbnail of Geolocation of AMSR-E Data

IEEE Transactions on Geoscience and Remote Sensing, 2008

Research paper thumbnail of Retrieval of sea ice emissivity and integrated retrieval of surface and atmospheric parameters over the arctic from AMSR-E data

Research paper thumbnail of Arctic Total Water Vapor: Comparison of Regional Climate Simulations with Observations, and Simulated Decadal Trends

Journal of Hydrometeorology, 2009

Satellite-retrieved data of total water vapor (TWV) over the Arctic are patchy, with large areas ... more Satellite-retrieved data of total water vapor (TWV) over the Arctic are patchy, with large areas of missing data because of various limitations of the retrieval algorithms. To overcome these observational difficulties, a new retrieval algorithm has been developed that allows for monitoring the TWV over the Arctic during most of the year. This method retrieves TWV from satellite microwave radiometer data [the Advanced Microwave Sounding Unit B (AMSU-B)]. These new data have been made available for 4 yr (2000–03) and have been used to evaluate high-resolution simulations with the Arctic regional atmospheric climate model HIRHAM at daily, monthly, and seasonal time scales. The strong dynamic TWV variability on the daily time scale, linked with moisture transport by weather systems, is discussed for selected case studies. Both the simulated climatological seasonal mean patterns and the variability on interannual and decadal time scales are in agreement with those of the 40-yr European C...

Research paper thumbnail of L-Band Radiometry for Sea-Ice Applications. Final Report for ESA ESTEC Contract 21130

Research paper thumbnail of Final Report IOMASA

Research paper thumbnail of 4.8 Sea ice emission modelling

Research paper thumbnail of Atmospheric and Surface Processes, and Feedback Mechanisms Determining Arctic Amplification: A Review of First Results and Prospects of the (AC)3 Project

Bulletin of the American Meteorological Society

Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To contribute to t... more Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To contribute to this debate, the (AC)3 project has been established in 2016 (http://www.ac3-tr.de/). It comprises modeling and data analysis efforts as well as observational elements. The project has assembled a wealth of ground-based, airborne, ship-borne, and satellite data of physical, chemical, and meteorological properties of the Arctic atmosphere, cryosphere, and upper ocean that are available for the Arctic climate research community. Short-term changes and indications of long-term trends in Arctic climate parameters have been detected using existing and new data. For example, a distinct atmospheric moistening, an increase of regional storm activities, an amplified winter warming in the Svalbard and North Pole regions, and a decrease of sea ice thickness in the Fram Strait and of snow depth on sea ice have been identified. A positive trend of tropospheric bromine monoxide (BrO) column densities du...

Research paper thumbnail of сравнительный анализ трёх моделей интертипных отношений в соционе

Соционика, ментология и психология личности, 2018

Research paper thumbnail of ESA Sea Ice Climate Change Initiative (Sea_Ice_cci): Sea Ice Concentration Climate Data Record from the AMSR-E and AMSR-2 instruments at 50 km grid spacing, version 2.0

Research paper thumbnail of RESOURCE: an International Initiative for Radio Sciences Research on Antarctic Atmosphere

Research paper thumbnail of Image restoration for SAM using computed optical transfer functions

Optik, 1994

A theory for surface structure imaging is presented, which allows the computation of optical tran... more A theory for surface structure imaging is presented, which allows the computation of optical transfer functions (OTF) of the scanning acoustic microscope (SAM). The model describes the monitor image in terms of the reflectivity of the specimen, thus including the influence of the confocal lens system and subsequent signal processing. Amplitude and phase contrast imaging in SAM are defined, and the corresponding OTF computed for different focus positions are shown to be in good agreement with measurements. Based on the theoretical OTF, an image restoration scheme for phase contrast imaging is developed. Combining images of a focal series, the imaging properties of SAM for phase contrast can be improved

Research paper thumbnail of Thickness of thin sea ice retrieved from SMOS and SMAP

2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS), 2016

Sea ice is an important quantity for the radiation budget of the Earth's climate system. In t... more Sea ice is an important quantity for the radiation budget of the Earth's climate system. In this paper we present a comparison of SMAP and SMOS measured brightness temperatures and translate a validated retrieval algorithm for the thickness of thin sea ice from SMOS to SMAP radiometer observations. For October to December all observations of SMAP in forward and backward direction are compared as daily averages and found with low RMSD of 2.25K and 2.42K in TB,v and TB,h, respectively. The mean of forward and backward observations from SMAP are mapped to SMOS equivalent brightness temperatures using a linear regression. SMAP was found to yield lower brightness temperatures compared to SMOS by about 5K in both polarizations while difference decreases with increasing brightness temperatures. An existing ice thickness retrieval for SMOS using averaged brightness temperatures in the incidence angles range of 40° to 50° is transferred to SMAP using another linear regression. Ice thickn...

Research paper thumbnail of Inter-comparison and evaluation of sea ice algorithms: towards further identification of challenges and optimal approach using passive microwave observations

Research paper thumbnail of Intertidal Topographic Maps and Morphological Changes in the German Wadden Sea between 1996–1999 and 2006–2009 from the Waterline Method and SAR Images

IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 2014

ABSTRACT The Dutch, German, and Danish Wadden Sea is one of the largest tidal flats in the world ... more ABSTRACT The Dutch, German, and Danish Wadden Sea is one of the largest tidal flats in the world which has been left in a nearly natural state. Several studies generated the topography of this valuable area, but presented only single maps, which covered partial regions of the Wadden Sea. The objectives of this paper are 1) to use the waterline method to analyze SAR images in order to generate annual topographic maps of the northern parts of the German Wadden Sea for the years 1996-1999 and 2006-2009 and 2) to quantitatively estimate and monitor the development of the tidal flats. The waterlines are detected by a wavelet-based edge detection algorithm, geocoded in Gauss-Krueger coordinates, assigned with water level information, and interpolated into topographic maps. Our results show the development of the tidal flats over the 8 years and illustrate three of the most changing regions: Tertiussand, Gelbsand, and Medemsand. Their area, shape, and sediment volume have changed significantly due to the tide, wave, wind, and river discharge influences. The waterline method is an efficient and economical way to monitor large tidal flat areas, which allows an estimation of long-term morphological development. One potential application is to assimilate the results into morphodynamic models in order to give finer morphological predictions.

Research paper thumbnail of Retrieval of total water vapor in polar regions using SSM/T2 channels

IGARSS'97. 1997 IEEE International Geoscience and Remote Sensing Symposium Proceedings. Remote Sensing - A Scientific Vision for Sustainable Development, 1997

ABSTRACT A method to retrieve the total water vapor in the cloudless atmosphere using SSM/T2 chan... more ABSTRACT A method to retrieve the total water vapor in the cloudless atmosphere using SSM/T2 channels is proposed based on a unique property of three contiguous channels situated on the flank of the water vapor absorption line at 183.31 GHz. One of its advantages is its independence to the surface emission, which is the main disturbing factor in retrieving atmospheric parameters from passive satellite measurements. Due to the high sensitivity of the SSM/T2 channels to water vapor, this method is suitable to the total water vapor retrieval for dry polar atmospheres. An algorithm is constructed for austral winter cases through model simulation using radiosonde profiles

Research paper thumbnail of New approach for radiative transfer in sea ice and its application for sea ice satellite remote sensing

ABSTRACT In this paper we present the newly developed analytical description of the radiative tra... more ABSTRACT In this paper we present the newly developed analytical description of the radiative transfer in the sea ice in visible and near IR region and the idea and first results of the retrieval of the melt pond fractions from data of a satellite spectral sensor. This retrieval is based on the analytical description of the optical properties of sea ice as a scattering medium.

Research paper thumbnail of Response of passive microwave sea ice concentration algorithms to thin ice

2014 IEEE Geoscience and Remote Sensing Symposium, 2014

The influence of sea ice thickness brightness temperatures and ice concentrations retrieved from ... more The influence of sea ice thickness brightness temperatures and ice concentrations retrieved from passive microwave observations is quantified, using horizontally homogeneous sea ice thickness retrievals from ESA's SMOS sensor observations at high incidence angles. Brightness temperatures are influenced by thickness below 18 cm (89GHz) and 50 cm (1.4 GHz). Ice concentration retrievals reduced by ice thickness below 0.17 m and 0.33 m, with higher frequency algorithms being less influenced.

Research paper thumbnail of Exploring Arctic Transpolar Drift During Dramatic Sea Ice Retreat

Eos, Transactions American Geophysical Union, 2008

Research paper thumbnail of AMS Journals Online - POLAR PROGRAM: Integrated

Research paper thumbnail of Comparison of Tropospheric Water Vapour over Antarctica Derived from AMSU-B Data, Ground-Based GPS Data and the NCEP/NCAR Reanalysis

Journal of the Meteorological Society of Japan, 2004

Research paper thumbnail of Geolocation of AMSR-E Data

IEEE Transactions on Geoscience and Remote Sensing, 2008

Research paper thumbnail of Retrieval of sea ice emissivity and integrated retrieval of surface and atmospheric parameters over the arctic from AMSR-E data

Research paper thumbnail of Arctic Total Water Vapor: Comparison of Regional Climate Simulations with Observations, and Simulated Decadal Trends

Journal of Hydrometeorology, 2009

Satellite-retrieved data of total water vapor (TWV) over the Arctic are patchy, with large areas ... more Satellite-retrieved data of total water vapor (TWV) over the Arctic are patchy, with large areas of missing data because of various limitations of the retrieval algorithms. To overcome these observational difficulties, a new retrieval algorithm has been developed that allows for monitoring the TWV over the Arctic during most of the year. This method retrieves TWV from satellite microwave radiometer data [the Advanced Microwave Sounding Unit B (AMSU-B)]. These new data have been made available for 4 yr (2000–03) and have been used to evaluate high-resolution simulations with the Arctic regional atmospheric climate model HIRHAM at daily, monthly, and seasonal time scales. The strong dynamic TWV variability on the daily time scale, linked with moisture transport by weather systems, is discussed for selected case studies. Both the simulated climatological seasonal mean patterns and the variability on interannual and decadal time scales are in agreement with those of the 40-yr European C...

Research paper thumbnail of L-Band Radiometry for Sea-Ice Applications. Final Report for ESA ESTEC Contract 21130

Research paper thumbnail of Final Report IOMASA

Research paper thumbnail of 4.8 Sea ice emission modelling