Daily microwave derived surface temperature over Canada/Alaska.

International audience The land surface temperature variation over northern high latitudes in response to the increase in greenhouse gases is challenging because of the lack of meteorological stations. A new method to derive the surface temperature from satellite microwave measurements that improves...

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Published in:Journal of Applied Meteorology and Climatology
Main Authors: Mialon, Arnaud, Royer, Alain, Fily, M., Picard, Ghislain
Other Authors: Centre d'Applications et de Recherches en TELédétection Sherbrooke (CARTEL), Département de géomatique appliquée Sherbrooke (UdeS), Université de Sherbrooke (UdeS)-Université de Sherbrooke (UdeS), Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
Ice
Online Access:https://hal.science/hal-00297819
https://hal.science/hal-00297819/document
https://hal.science/hal-00297819/file/%5B15588432%20-%20Journal%20of%20Applied%20Meteorology%20and%20Climatology%5D%20Daily%20Microwave-Derived%20Surface%20Temperature%20over%20Canada_Alaska.pdf
https://doi.org/10.1175/JAM2485.1
id ftinsu:oai:HAL:hal-00297819v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic passive microwave
remote sensing data (SSM/I)
surface temperature
high latitudes
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle passive microwave
remote sensing data (SSM/I)
surface temperature
high latitudes
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Mialon, Arnaud
Royer, Alain
Fily, M.
Picard, Ghislain
Daily microwave derived surface temperature over Canada/Alaska.
topic_facet passive microwave
remote sensing data (SSM/I)
surface temperature
high latitudes
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience The land surface temperature variation over northern high latitudes in response to the increase in greenhouse gases is challenging because of the lack of meteorological stations. A new method to derive the surface temperature from satellite microwave measurements that improves the frequency of measurements relative to that of infrared data is presented. The daily Special Sensor Microwave Imager 25 km × 25 km Equal-Area Scalable Earth Grid (EASE-Grid) dataset provided by the National Snow and Ice Data Center in Boulder, Colorado, is processed to derive the surface temperature using the method proposed by Fily et al. A normalization approach based on the 40-yr ECMWF reanalysis (ERA-40; 2.5°) temperature diurnal cycle fitted for each pixel is applied to overcome the time acquisition variation of measurements as well as to interpolate missing data. An adaptive mask for discriminating between ice-free pixels and snow-free pixels is also applied. The resulting database is thus a new consistent hourly series of near-surface air temperatures during the summer (without snow). The mean accuracy is on the order of 2.5–3 K when compared with the synchronous in situ air temperature and different gridded datasets over Canada and Alaska. The trend over the last 10 yr confirms observed climate evolution: an increase in summer surface temperature of +0.09° ± 0.04°C yr−1, at the 90% confidence level, for Canada between 1992 and 2002, whereas a decrease of −0.15° ± 0.05°C yr−1, at the 95% confidence level, is observed for Alaska. Spatial and temporal anomalies show regional impacts of meteorological phenomena such as the El Niño extreme warm summer episode of 1998, the decrease in temperatures in 1992 in Canada following the volcanic eruption of Mount Pinatubo in June 1991, and the strong drought in the prairies in 2001. The annual sum of positive degree-days (thawing index) has been related to the permafrost distribution. The lower values of the derived thawing index (<1400 degree-days) are related ...
author2 Centre d'Applications et de Recherches en TELédétection Sherbrooke (CARTEL)
Département de géomatique appliquée Sherbrooke (UdeS)
Université de Sherbrooke (UdeS)-Université de Sherbrooke (UdeS)
Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Mialon, Arnaud
Royer, Alain
Fily, M.
Picard, Ghislain
author_facet Mialon, Arnaud
Royer, Alain
Fily, M.
Picard, Ghislain
author_sort Mialon, Arnaud
title Daily microwave derived surface temperature over Canada/Alaska.
title_short Daily microwave derived surface temperature over Canada/Alaska.
title_full Daily microwave derived surface temperature over Canada/Alaska.
title_fullStr Daily microwave derived surface temperature over Canada/Alaska.
title_full_unstemmed Daily microwave derived surface temperature over Canada/Alaska.
title_sort daily microwave derived surface temperature over canada/alaska.
publisher HAL CCSD
publishDate 2007
url https://hal.science/hal-00297819
https://hal.science/hal-00297819/document
https://hal.science/hal-00297819/file/%5B15588432%20-%20Journal%20of%20Applied%20Meteorology%20and%20Climatology%5D%20Daily%20Microwave-Derived%20Surface%20Temperature%20over%20Canada_Alaska.pdf
https://doi.org/10.1175/JAM2485.1
genre Ice
National Snow and Ice Data Center
permafrost
Alaska
genre_facet Ice
National Snow and Ice Data Center
permafrost
Alaska
op_source ISSN: 1558-8424
EISSN: 1558-8432
Journal of Applied Meteorology and Climatology
https://hal.science/hal-00297819
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https://hal.science/hal-00297819
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doi:10.1175/JAM2485.1
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1175/JAM2485.1
container_title Journal of Applied Meteorology and Climatology
container_volume 46
container_issue 5
container_start_page 591
op_container_end_page 604
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spelling ftinsu:oai:HAL:hal-00297819v1 2024-04-28T08:23:53+00:00 Daily microwave derived surface temperature over Canada/Alaska. Mialon, Arnaud Royer, Alain Fily, M. Picard, Ghislain Centre d'Applications et de Recherches en TELédétection Sherbrooke (CARTEL) Département de géomatique appliquée Sherbrooke (UdeS) Université de Sherbrooke (UdeS)-Université de Sherbrooke (UdeS) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) 2007-05 https://hal.science/hal-00297819 https://hal.science/hal-00297819/document https://hal.science/hal-00297819/file/%5B15588432%20-%20Journal%20of%20Applied%20Meteorology%20and%20Climatology%5D%20Daily%20Microwave-Derived%20Surface%20Temperature%20over%20Canada_Alaska.pdf https://doi.org/10.1175/JAM2485.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JAM2485.1 hal-00297819 https://hal.science/hal-00297819 https://hal.science/hal-00297819/document https://hal.science/hal-00297819/file/%5B15588432%20-%20Journal%20of%20Applied%20Meteorology%20and%20Climatology%5D%20Daily%20Microwave-Derived%20Surface%20Temperature%20over%20Canada_Alaska.pdf doi:10.1175/JAM2485.1 info:eu-repo/semantics/OpenAccess ISSN: 1558-8424 EISSN: 1558-8432 Journal of Applied Meteorology and Climatology https://hal.science/hal-00297819 Journal of Applied Meteorology and Climatology, 2007, 46 (5), pp.591-604. &#x27E8;10.1175/JAM2485.1&#x27E9; passive microwave remote sensing data (SSM/I) surface temperature high latitudes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2007 ftinsu https://doi.org/10.1175/JAM2485.1 2024-04-05T00:38:11Z International audience The land surface temperature variation over northern high latitudes in response to the increase in greenhouse gases is challenging because of the lack of meteorological stations. A new method to derive the surface temperature from satellite microwave measurements that improves the frequency of measurements relative to that of infrared data is presented. The daily Special Sensor Microwave Imager 25 km × 25 km Equal-Area Scalable Earth Grid (EASE-Grid) dataset provided by the National Snow and Ice Data Center in Boulder, Colorado, is processed to derive the surface temperature using the method proposed by Fily et al. A normalization approach based on the 40-yr ECMWF reanalysis (ERA-40; 2.5°) temperature diurnal cycle fitted for each pixel is applied to overcome the time acquisition variation of measurements as well as to interpolate missing data. An adaptive mask for discriminating between ice-free pixels and snow-free pixels is also applied. The resulting database is thus a new consistent hourly series of near-surface air temperatures during the summer (without snow). The mean accuracy is on the order of 2.5–3 K when compared with the synchronous in situ air temperature and different gridded datasets over Canada and Alaska. The trend over the last 10 yr confirms observed climate evolution: an increase in summer surface temperature of +0.09° ± 0.04°C yr−1, at the 90% confidence level, for Canada between 1992 and 2002, whereas a decrease of −0.15° ± 0.05°C yr−1, at the 95% confidence level, is observed for Alaska. Spatial and temporal anomalies show regional impacts of meteorological phenomena such as the El Niño extreme warm summer episode of 1998, the decrease in temperatures in 1992 in Canada following the volcanic eruption of Mount Pinatubo in June 1991, and the strong drought in the prairies in 2001. The annual sum of positive degree-days (thawing index) has been related to the permafrost distribution. The lower values of the derived thawing index (<1400 degree-days) are related ... Article in Journal/Newspaper Ice National Snow and Ice Data Center permafrost Alaska Institut national des sciences de l'Univers: HAL-INSU Journal of Applied Meteorology and Climatology 46 5 591 604