High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements

Short abstract From 15th May to 11th October 2019, six Saildrone autonomous surface vehicles (ASVs) were deployed for 150-day cruises collecting a suite of atmospheric and oceanographic measurements from Dutch Harbor, Alaska, transiting the Bering Strait into the Chukchi Sea. Two Saildrones funded b...

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Main Author: Chong Jia
Format: Lecture
Language:unknown
Published: Zenodo 2022
Subjects:
Online Access:https://doi.org/10.5281/zenodo.7259096
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spelling ftzenodo:oai:zenodo.org:7259096 2024-09-15T17:59:43+00:00 High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements Chong Jia 2022-06-27 https://doi.org/10.5281/zenodo.7259096 unknown Zenodo https://zenodo.org/communities/ghrsst https://doi.org/10.5281/zenodo.7259095 https://doi.org/10.5281/zenodo.7259096 oai:zenodo.org:7259096 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/lecture 2022 ftzenodo https://doi.org/10.5281/zenodo.725909610.5281/zenodo.7259095 2024-07-26T15:20:15Z Short abstract From 15th May to 11th October 2019, six Saildrone autonomous surface vehicles (ASVs) were deployed for 150-day cruises collecting a suite of atmospheric and oceanographic measurements from Dutch Harbor, Alaska, transiting the Bering Strait into the Chukchi Sea. Two Saildrones funded by NASA (the National Aeronautics and Space Administration), SD-1036 and SD-1037, were equipped with infrared pyrometers in a “unicorn” structure on the deck for the determination of the ocean sea-surface skin temperature (SSTskin). We present an algorithm to derive SSTskin from the downward- and upward-looking radiometers and estimate the main contributions to inaccuracy of the SSTskin. After stringent quality control of data and eliminating measurements influenced by sea ice and precipitation, and restricting the acceptable tilt angle of the ASV based on line-by-line radiative transfer model (LBLRTM) simulations, SSTskin can be derived to an accuracy of 0.12 K. The error budget of the derived SSTskin is developed and the largest component comes from the instrumental uncertainties assuming the viewing geometry is adequately determined. Thus, Saildrones equipped with these sensors could provide sufficiently accurate SSTskin retrievals for studying the physics of the thermal skin effect, in conjunction with accurate sub-surface thermometer measurements, and for validating satellite-derived SSTskin at high latitudes. Lecture Bering Strait Chukchi Chukchi Sea Sea ice Alaska Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description Short abstract From 15th May to 11th October 2019, six Saildrone autonomous surface vehicles (ASVs) were deployed for 150-day cruises collecting a suite of atmospheric and oceanographic measurements from Dutch Harbor, Alaska, transiting the Bering Strait into the Chukchi Sea. Two Saildrones funded by NASA (the National Aeronautics and Space Administration), SD-1036 and SD-1037, were equipped with infrared pyrometers in a “unicorn” structure on the deck for the determination of the ocean sea-surface skin temperature (SSTskin). We present an algorithm to derive SSTskin from the downward- and upward-looking radiometers and estimate the main contributions to inaccuracy of the SSTskin. After stringent quality control of data and eliminating measurements influenced by sea ice and precipitation, and restricting the acceptable tilt angle of the ASV based on line-by-line radiative transfer model (LBLRTM) simulations, SSTskin can be derived to an accuracy of 0.12 K. The error budget of the derived SSTskin is developed and the largest component comes from the instrumental uncertainties assuming the viewing geometry is adequately determined. Thus, Saildrones equipped with these sensors could provide sufficiently accurate SSTskin retrievals for studying the physics of the thermal skin effect, in conjunction with accurate sub-surface thermometer measurements, and for validating satellite-derived SSTskin at high latitudes.
format Lecture
author Chong Jia
spellingShingle Chong Jia
High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements
author_facet Chong Jia
author_sort Chong Jia
title High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements
title_short High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements
title_full High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements
title_fullStr High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements
title_full_unstemmed High Latitude Sea-Surface Skin Temperatures Derived from Saildrone Infrared Measurements
title_sort high latitude sea-surface skin temperatures derived from saildrone infrared measurements
publisher Zenodo
publishDate 2022
url https://doi.org/10.5281/zenodo.7259096
genre Bering Strait
Chukchi
Chukchi Sea
Sea ice
Alaska
genre_facet Bering Strait
Chukchi
Chukchi Sea
Sea ice
Alaska
op_relation https://zenodo.org/communities/ghrsst
https://doi.org/10.5281/zenodo.7259095
https://doi.org/10.5281/zenodo.7259096
oai:zenodo.org:7259096
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.725909610.5281/zenodo.7259095
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