Improved Arctic sea-ice motion in summer from the brightness temperature of the AMSR2 36GHz channel

Author:

Shi Qian1ORCID,Yang Qinghua1ORCID,Su Jie2ORCID,Liu Jiping1,Sun Qizhen3

Affiliation:

1. School of Atmospheric Sciences, Sun Yat-sen University, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, People’s Republic of China

2. Frontier Science Center for Deep Ocean Multispheres and Earth System (FDMES) Physical Oceanography Laboratory, Ocean University of China, Qingdao, People’s Republic of China

3. National Marine Environmental Forecasting Center, Beijing, People’s Republic of China

Funder

National Natural Science Foundation of China

fundamental research funds for the Norges Forskningsråd

Publisher

Informa UK Limited

Reference31 articles.

1. Baordo F. L. F. Vargas and E. Howe. 2023. “OSI SAF Product User Manual for Global Sea Ice Concentration Level 2 and Level 3 OSI-410-a OSI-401-d OSI-408-a. Version 1 1/11/2022.” Available online: https://osisaf-hl.met.no/sites/osisaf-hl/files/user_manuals/osisaf_pum_ice-conc_l2-3_v1p0.pdf.

2. Determination of sea ice parameters with the NIMBUS 7 SMMR

3. Ezraty Robert Fanny Girard-Ardhuin and Jean-François Piollé. 2007. Sea Ice Drift in the Central Arctic Estimated From Seawinds/Quikscat Backscatter Maps User’s Manual .

4. Validation of remote-sensing products of sea-ice motion: a case study in the western Arctic Ocean

5. Comparing L- and C-band synthetic aperture radar estimates of sea ice motion over different ice regimes

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