Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model

DMRT-ML is a physically based numerical model designed to compute the thermal microwave emission of a given snowpack. Its main application is the simulation of brightness temperatures at frequencies in the range 1–200 GHz similar to those acquired routinely by space-based microwave radiometers. The...

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Published in:Geoscientific Model Development
Main Authors: G. Picard, L. Brucker, A. Roy, F. Dupont, M. Fily, A. Royer, C. Harlow
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/gmd-6-1061-2013
https://doaj.org/article/7987f35e58d04b8abc9d02b9ef991597
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spelling ftdoajarticles:oai:doaj.org/article:7987f35e58d04b8abc9d02b9ef991597 2023-05-15T13:49:08+02:00 Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model G. Picard L. Brucker A. Roy F. Dupont M. Fily A. Royer C. Harlow 2013-07-01T00:00:00Z https://doi.org/10.5194/gmd-6-1061-2013 https://doaj.org/article/7987f35e58d04b8abc9d02b9ef991597 EN eng Copernicus Publications http://www.geosci-model-dev.net/6/1061/2013/gmd-6-1061-2013.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 doi:10.5194/gmd-6-1061-2013 1991-959X 1991-9603 https://doaj.org/article/7987f35e58d04b8abc9d02b9ef991597 Geoscientific Model Development, Vol 6, Iss 4, Pp 1061-1078 (2013) Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/gmd-6-1061-2013 2022-12-30T22:55:47Z DMRT-ML is a physically based numerical model designed to compute the thermal microwave emission of a given snowpack. Its main application is the simulation of brightness temperatures at frequencies in the range 1–200 GHz similar to those acquired routinely by space-based microwave radiometers. The model is based on the Dense Media Radiative Transfer (DMRT) theory for the computation of the snow scattering and extinction coefficients and on the Discrete Ordinate Method (DISORT) to numerically solve the radiative transfer equation. The snowpack is modeled as a stack of multiple horizontal snow layers and an optional underlying interface representing the soil or the bottom ice. The model handles both dry and wet snow conditions. Such a general design allows the model to account for a wide range of snow conditions. Hitherto, the model has been used to simulate the thermal emission of the deep firn on ice sheets, shallow snowpacks overlying soil in Arctic and Alpine regions, and overlying ice on the large ice-sheet margins and glaciers. DMRT-ML has thus been validated in three very different conditions: Antarctica, Barnes Ice Cap (Canada) and Canadian tundra. It has been recently used in conjunction with inverse methods to retrieve snow grain size from remote sensing data. The model is written in Fortran90 and available to the snow remote sensing community as an open-source software. A convenient user interface is provided in Python. Article in Journal/Newspaper Antarc* Antarctica Arctic Barnes Ice Cap glacier* Ice cap Ice Sheet Tundra Directory of Open Access Journals: DOAJ Articles Arctic Canada Barnes Ice Cap ENVELOPE(-73.498,-73.498,70.001,70.001) Geoscientific Model Development 6 4 1061 1078
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
G. Picard
L. Brucker
A. Roy
F. Dupont
M. Fily
A. Royer
C. Harlow
Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model
topic_facet Geology
QE1-996.5
description DMRT-ML is a physically based numerical model designed to compute the thermal microwave emission of a given snowpack. Its main application is the simulation of brightness temperatures at frequencies in the range 1–200 GHz similar to those acquired routinely by space-based microwave radiometers. The model is based on the Dense Media Radiative Transfer (DMRT) theory for the computation of the snow scattering and extinction coefficients and on the Discrete Ordinate Method (DISORT) to numerically solve the radiative transfer equation. The snowpack is modeled as a stack of multiple horizontal snow layers and an optional underlying interface representing the soil or the bottom ice. The model handles both dry and wet snow conditions. Such a general design allows the model to account for a wide range of snow conditions. Hitherto, the model has been used to simulate the thermal emission of the deep firn on ice sheets, shallow snowpacks overlying soil in Arctic and Alpine regions, and overlying ice on the large ice-sheet margins and glaciers. DMRT-ML has thus been validated in three very different conditions: Antarctica, Barnes Ice Cap (Canada) and Canadian tundra. It has been recently used in conjunction with inverse methods to retrieve snow grain size from remote sensing data. The model is written in Fortran90 and available to the snow remote sensing community as an open-source software. A convenient user interface is provided in Python.
format Article in Journal/Newspaper
author G. Picard
L. Brucker
A. Roy
F. Dupont
M. Fily
A. Royer
C. Harlow
author_facet G. Picard
L. Brucker
A. Roy
F. Dupont
M. Fily
A. Royer
C. Harlow
author_sort G. Picard
title Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model
title_short Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model
title_full Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model
title_fullStr Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model
title_full_unstemmed Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model
title_sort simulation of the microwave emission of multi-layered snowpacks using the dense media radiative transfer theory: the dmrt-ml model
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/gmd-6-1061-2013
https://doaj.org/article/7987f35e58d04b8abc9d02b9ef991597
long_lat ENVELOPE(-73.498,-73.498,70.001,70.001)
geographic Arctic
Canada
Barnes Ice Cap
geographic_facet Arctic
Canada
Barnes Ice Cap
genre Antarc*
Antarctica
Arctic
Barnes Ice Cap
glacier*
Ice cap
Ice Sheet
Tundra
genre_facet Antarc*
Antarctica
Arctic
Barnes Ice Cap
glacier*
Ice cap
Ice Sheet
Tundra
op_source Geoscientific Model Development, Vol 6, Iss 4, Pp 1061-1078 (2013)
op_relation http://www.geosci-model-dev.net/6/1061/2013/gmd-6-1061-2013.pdf
https://doaj.org/toc/1991-959X
https://doaj.org/toc/1991-9603
doi:10.5194/gmd-6-1061-2013
1991-959X
1991-9603
https://doaj.org/article/7987f35e58d04b8abc9d02b9ef991597
op_doi https://doi.org/10.5194/gmd-6-1061-2013
container_title Geoscientific Model Development
container_volume 6
container_issue 4
container_start_page 1061
op_container_end_page 1078
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