French Polar Institute Literature Database
Home
|
Show All
|
Simple Search
|
Advanced Search
Login
Quick Search:
Field:
main fields
author
title
publication
keywords
abstract
programme
type
contains:
...
1–1 of 1 record found matching your query (
RSS
|
history
):
Search within Results:
Field:
author
title
year
keywords
abstract
programme
type
publication
abbrev_journal
volume
issue
pages
publisher
place
editor
series_title
language
area
notes
contains:
...
Exclude matches
Display Options:
Field:
all fields
keywords & abstract
additional fields
records per page
Select All
Deselect All
<<
1
>>
List View
|
Citations
|
Details
Record
Links
Author
Marion Leduc-Leballeur, Ghislain Picard, Giovanni Macelloni, Arnaud Mialon, Yann H. Kerr
Title
Melt in Antarctica derived from Soil Moisture and Ocean Salinity (SMOS) observations at L band
Type
Journal
Year
2020
Publication
The Cryosphere
Abbreviated Journal
Volume
14
Issue
2
Pages
539-548
Keywords
Abstract
Melt occurrence in Antarctica is derived from L-band observations from the Soil Moisture and Ocean Salinity (SMOS) satellite between the austral summer 2010–2011 and 2017–2018. The detection algorithm is adapted from a threshold method previously developed for 19 GHz passive microwave measurements from the special sensor microwave imager (SSM/I) and special sensor microwave imager sounder (SSMIS). The comparison of daily melt occurrence retrieved from 1.4 and 19 GHz observations shows an overall close agreement, but a lag of few days is usually observed by SMOS at the beginning of the melt season. To understand the difference, a theoretical analysis is performed using a microwave emission radiative transfer model. It shows that the sensitivity of 1.4 GHz signal to liquid water is significantly weaker than at 19 GHz if the water is only present in the uppermost tens of centimetres of the snowpack. Conversely, 1.4 GHz measurements are sensitive to water when spread over at least 1 m and when present in depths up to hundreds of metres. This is explained by the large penetration depth in dry snow and by the long wavelength (21 cm). We conclude that SMOS and higher-frequency radiometers provide interesting complementary information on melt occurrence and on the location of the water in the snowpack.
Programme
1110
Campaign
Address
Corporate Author
Thesis
Publisher
Place of Publication
Editor
Language
Summary Language
Original Title
Series Editor
Series Title
Abbreviated Series Title
Series Volume
Series Issue
Edition
ISSN
1994-0416
ISBN
Medium
Area
Expedition
Conference
Notes
Approved
yes
Call Number
Serial
7689
Permanent link to this record
Select All
Deselect All
<<
1
>>
List View
|
Citations
|
Details
Home
Show Record
|
Help