ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis

Non-lag and lag correlation coefficients between Niño 3 indices derived from sea-surface temperature (SST) anomalies and land surface variables from satellite based Moderate Resolution Imaging Spectroradiometer (MODIS) data, as well as National Center for Environmental Prediction/National Center for...

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Main Authors: Henry Bartholomew, Menglin S. Jin
Format: Article
Language:English
Published: MDPI AG 2013-08-01
Series:Climate
Subjects:
Online Access:http://www.mdpi.com/2225-1154/1/2/53
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spelling doaj-30bf7fd1419f414b9c553c3c3960e6422020-11-24T22:41:52ZengMDPI AGClimate2225-11542013-08-0112537310.3390/cli1020053ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR ReanalysisHenry BartholomewMenglin S. JinNon-lag and lag correlation coefficients between Niño 3 indices derived from sea-surface temperature (SST) anomalies and land surface variables from satellite based Moderate Resolution Imaging Spectroradiometer (MODIS) data, as well as National Center for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) Reanalysis data are analyzed for 2001–2010. Strong positive correlations between January Niño 3 indices and skin temperature (Tskin) occur over the northwest USA, western Canada, and southern Alaska, suggesting that an El Niño event is associated with warmer winter temperatures over these regions, consistent with previous studies based on 2 m surface air temperature measurements (Tair). In addition, in January, strong negative correlations exist over central and northern Europe (meaning colder than normal winters) with positive correlations present over central Siberia (suggesting warmer than normal winters). Despite the different physical meaning between Tair and Tskin, the general response of the two surface temperatures to changes in ENSO is similar. Nevertheless, satellite observations of Tskin provide more rich information and higher spatial resolution than Tair data.http://www.mdpi.com/2225-1154/1/2/53MODISskin temperatureair temperatureEl NiñoENSONCEP/NCAR
collection DOAJ
language English
format Article
sources DOAJ
author Henry Bartholomew
Menglin S. Jin
spellingShingle Henry Bartholomew
Menglin S. Jin
ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis
Climate
MODIS
skin temperature
air temperature
El Niño
ENSO
NCEP/NCAR
author_facet Henry Bartholomew
Menglin S. Jin
author_sort Henry Bartholomew
title ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis
title_short ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis
title_full ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis
title_fullStr ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis
title_full_unstemmed ENSO Effects on Land Skin Temperature Variations: A Global Study from Satellite Remote Sensing and NCEP/NCAR Reanalysis
title_sort enso effects on land skin temperature variations: a global study from satellite remote sensing and ncep/ncar reanalysis
publisher MDPI AG
series Climate
issn 2225-1154
publishDate 2013-08-01
description Non-lag and lag correlation coefficients between Niño 3 indices derived from sea-surface temperature (SST) anomalies and land surface variables from satellite based Moderate Resolution Imaging Spectroradiometer (MODIS) data, as well as National Center for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) Reanalysis data are analyzed for 2001–2010. Strong positive correlations between January Niño 3 indices and skin temperature (Tskin) occur over the northwest USA, western Canada, and southern Alaska, suggesting that an El Niño event is associated with warmer winter temperatures over these regions, consistent with previous studies based on 2 m surface air temperature measurements (Tair). In addition, in January, strong negative correlations exist over central and northern Europe (meaning colder than normal winters) with positive correlations present over central Siberia (suggesting warmer than normal winters). Despite the different physical meaning between Tair and Tskin, the general response of the two surface temperatures to changes in ENSO is similar. Nevertheless, satellite observations of Tskin provide more rich information and higher spatial resolution than Tair data.
topic MODIS
skin temperature
air temperature
El Niño
ENSO
NCEP/NCAR
url http://www.mdpi.com/2225-1154/1/2/53
work_keys_str_mv AT henrybartholomew ensoeffectsonlandskintemperaturevariationsaglobalstudyfromsatelliteremotesensingandncepncarreanalysis
AT menglinsjin ensoeffectsonlandskintemperaturevariationsaglobalstudyfromsatelliteremotesensingandncepncarreanalysis
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