Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions.
The figure illustrates the sensitivities of the low passive microwave brightness temperature at the top-of-the-atmosphere, in terms of Sea Surface Temperature (SST), Sea Surface Salinity (SSS), Ocean Wind Speed (OWS) and Sea Ice Concentration (SIC) as a function of frequency from 1 to 40 GHz. The Co...
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ftdatacite:10.6084/m9.figshare.11709765.v1 2023-05-15T14:56:10+02:00 Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. Kilic, Lise Prigent, Catherine Jimenez, Carlos 2020 https://dx.doi.org/10.6084/m9.figshare.11709765.v1 https://figshare.com/articles/Sensitivities_to_ocean_and_sea_ice_parameters_as_a_function_of_CIMR_channels_for_arctic_mid-latitude_and_tropical_conditions_/11709765/1 unknown figshare https://dx.doi.org/10.6084/m9.figshare.11709765 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Oceanography FOS Earth and related environmental sciences Environmental Science 49999 Earth Sciences not elsewhere classified 40107 Meteorology Image Figure graphic ImageObject 2020 ftdatacite https://doi.org/10.6084/m9.figshare.11709765.v1 https://doi.org/10.6084/m9.figshare.11709765 2021-11-05T12:55:41Z The figure illustrates the sensitivities of the low passive microwave brightness temperature at the top-of-the-atmosphere, in terms of Sea Surface Temperature (SST), Sea Surface Salinity (SSS), Ocean Wind Speed (OWS) and Sea Ice Concentration (SIC) as a function of frequency from 1 to 40 GHz. The Copernicus Imaging Microwave Radiometer (CIMR) channels are indicated at the top of the figure. Three different geophysical conditions are considered: arctic, mid-latitude and tropical. For each parameter the sensitivity is normalized by the maximum of sensitivity between the three considered environments, for the full frequency range from 1 to 40 GHz. The sensitivities have been computed using the ocean radiative transfer model of Remote Sensing Systems (Meissner and Wentz, 2012), the sea ice emissivities estimated from the ESA sea ice Round Robin Data Package (Pedersen et al., 2019), and the atmospheric radiative transfer model of Rosenkranz (Rosenkranz, 2017). Still Image Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Pedersen ENVELOPE(140.013,140.013,-66.668,-66.668) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Oceanography FOS Earth and related environmental sciences Environmental Science 49999 Earth Sciences not elsewhere classified 40107 Meteorology |
spellingShingle |
Oceanography FOS Earth and related environmental sciences Environmental Science 49999 Earth Sciences not elsewhere classified 40107 Meteorology Kilic, Lise Prigent, Catherine Jimenez, Carlos Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. |
topic_facet |
Oceanography FOS Earth and related environmental sciences Environmental Science 49999 Earth Sciences not elsewhere classified 40107 Meteorology |
description |
The figure illustrates the sensitivities of the low passive microwave brightness temperature at the top-of-the-atmosphere, in terms of Sea Surface Temperature (SST), Sea Surface Salinity (SSS), Ocean Wind Speed (OWS) and Sea Ice Concentration (SIC) as a function of frequency from 1 to 40 GHz. The Copernicus Imaging Microwave Radiometer (CIMR) channels are indicated at the top of the figure. Three different geophysical conditions are considered: arctic, mid-latitude and tropical. For each parameter the sensitivity is normalized by the maximum of sensitivity between the three considered environments, for the full frequency range from 1 to 40 GHz. The sensitivities have been computed using the ocean radiative transfer model of Remote Sensing Systems (Meissner and Wentz, 2012), the sea ice emissivities estimated from the ESA sea ice Round Robin Data Package (Pedersen et al., 2019), and the atmospheric radiative transfer model of Rosenkranz (Rosenkranz, 2017). |
format |
Still Image |
author |
Kilic, Lise Prigent, Catherine Jimenez, Carlos |
author_facet |
Kilic, Lise Prigent, Catherine Jimenez, Carlos |
author_sort |
Kilic, Lise |
title |
Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. |
title_short |
Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. |
title_full |
Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. |
title_fullStr |
Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. |
title_full_unstemmed |
Sensitivities to ocean and sea ice parameters as a function of CIMR channels for arctic, mid-latitude, and tropical conditions. |
title_sort |
sensitivities to ocean and sea ice parameters as a function of cimr channels for arctic, mid-latitude, and tropical conditions. |
publisher |
figshare |
publishDate |
2020 |
url |
https://dx.doi.org/10.6084/m9.figshare.11709765.v1 https://figshare.com/articles/Sensitivities_to_ocean_and_sea_ice_parameters_as_a_function_of_CIMR_channels_for_arctic_mid-latitude_and_tropical_conditions_/11709765/1 |
long_lat |
ENVELOPE(140.013,140.013,-66.668,-66.668) |
geographic |
Arctic Pedersen |
geographic_facet |
Arctic Pedersen |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_relation |
https://dx.doi.org/10.6084/m9.figshare.11709765 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.11709765.v1 https://doi.org/10.6084/m9.figshare.11709765 |
_version_ |
1766328199894007808 |