Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica

The firn temperature is a crucial parameter for understanding firn densification processes of the Antarctic Ice Sheet (AIS). Simulations with firn densification models (FDM) can be conceptualized as a function that relies on forcing data, comprising temperature and surface mass balance, together wit...

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Published in:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Main Authors: Wang, Xiaofeng, An, Lu, Langen, Peter L., Li, Rongxing
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/isprs-archives-XLVIII-1-2024-691-2024
https://isprs-archives.copernicus.org/articles/XLVIII-1-2024/691/2024/
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spelling ftcopernicus:oai:publications.copernicus.org:isprs-archives120164 2024-06-23T07:47:01+00:00 Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica Wang, Xiaofeng An, Lu Langen, Peter L. Li, Rongxing 2024-05-11 application/pdf https://doi.org/10.5194/isprs-archives-XLVIII-1-2024-691-2024 https://isprs-archives.copernicus.org/articles/XLVIII-1-2024/691/2024/ eng eng doi:10.5194/isprs-archives-XLVIII-1-2024-691-2024 https://isprs-archives.copernicus.org/articles/XLVIII-1-2024/691/2024/ eISSN: 2194-9034 Text 2024 ftcopernicus https://doi.org/10.5194/isprs-archives-XLVIII-1-2024-691-2024 2024-06-13T01:24:45Z The firn temperature is a crucial parameter for understanding firn densification processes of the Antarctic Ice Sheet (AIS). Simulations with firn densification models (FDM) can be conceptualized as a function that relies on forcing data, comprising temperature and surface mass balance, together with tuning parameters determined based on measured depth-density profiles from different locations. The simulated firn temperature is obtained in the firn densification models by solving the one-dimensional heat conduction equation. Microwave satellite data on brightness temperature at different frequencies can also provide remote sensing monitoring of firn temperature variations across the AIS (i.e., the L-band up to 1500 meters). The firn temperature can be estimated by the microwave emission model and the regression method, but these two methods need more observations of temperature profiles for correction and validation. Therefore, we compiled a dataset with temperature profiles and temperature observations with depth around 10 meters. In this work, two methods were used to simulate/retrieve firn temperature across the Antarctic ice sheet. One method estimated the temperature profiles by solving the one-dimensional heat conduction equation driven by reanalyses and regional climate models, which are used in the simulation of FDMs. The other one established a relationship between the multi-frequency brightness temperature data from microwave remote sensing satellites and the firn temperature. Text Antarc* Antarctic Antarctica Ice Sheet Copernicus Publications: E-Journals Antarctic The Antarctic The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLVIII-1-2024 691 696
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The firn temperature is a crucial parameter for understanding firn densification processes of the Antarctic Ice Sheet (AIS). Simulations with firn densification models (FDM) can be conceptualized as a function that relies on forcing data, comprising temperature and surface mass balance, together with tuning parameters determined based on measured depth-density profiles from different locations. The simulated firn temperature is obtained in the firn densification models by solving the one-dimensional heat conduction equation. Microwave satellite data on brightness temperature at different frequencies can also provide remote sensing monitoring of firn temperature variations across the AIS (i.e., the L-band up to 1500 meters). The firn temperature can be estimated by the microwave emission model and the regression method, but these two methods need more observations of temperature profiles for correction and validation. Therefore, we compiled a dataset with temperature profiles and temperature observations with depth around 10 meters. In this work, two methods were used to simulate/retrieve firn temperature across the Antarctic ice sheet. One method estimated the temperature profiles by solving the one-dimensional heat conduction equation driven by reanalyses and regional climate models, which are used in the simulation of FDMs. The other one established a relationship between the multi-frequency brightness temperature data from microwave remote sensing satellites and the firn temperature.
format Text
author Wang, Xiaofeng
An, Lu
Langen, Peter L.
Li, Rongxing
spellingShingle Wang, Xiaofeng
An, Lu
Langen, Peter L.
Li, Rongxing
Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica
author_facet Wang, Xiaofeng
An, Lu
Langen, Peter L.
Li, Rongxing
author_sort Wang, Xiaofeng
title Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica
title_short Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica
title_full Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica
title_fullStr Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica
title_full_unstemmed Comparing firn temperature profile retrieval based on the firn densification model and microwave data over the Antarctica
title_sort comparing firn temperature profile retrieval based on the firn densification model and microwave data over the antarctica
publishDate 2024
url https://doi.org/10.5194/isprs-archives-XLVIII-1-2024-691-2024
https://isprs-archives.copernicus.org/articles/XLVIII-1-2024/691/2024/
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_source eISSN: 2194-9034
op_relation doi:10.5194/isprs-archives-XLVIII-1-2024-691-2024
https://isprs-archives.copernicus.org/articles/XLVIII-1-2024/691/2024/
op_doi https://doi.org/10.5194/isprs-archives-XLVIII-1-2024-691-2024
container_title The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
container_volume XLVIII-1-2024
container_start_page 691
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