Decadal surface temperature trends in India based on a new high-resolution data set

Abstract A new comprehensive surface temperature data set for India is used to document changes in Indian temperature over seven decades, in order to examine the patterns and possible effects of global warming. The data set is subdivided into pre-monsoon, monsoon, and post-monsoon categories in orde...

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Main Authors: Robert S. Ross, T. N. Krishnamurti, Sandeep Pattnaik, D. S. Pai
Format: Article
Language:English
Published: Nature Publishing Group 2018-05-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-018-25347-2
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spelling doaj-3d4a892dcc9f422d9a9662e345a4a0582020-12-08T03:29:39ZengNature Publishing GroupScientific Reports2045-23222018-05-018111010.1038/s41598-018-25347-2Decadal surface temperature trends in India based on a new high-resolution data setRobert S. Ross0T. N. Krishnamurti1Sandeep Pattnaik2D. S. Pai3Department of Earth, Ocean and Atmospheric Science, Florida State UniversityDepartment of Earth, Ocean and Atmospheric Science, Florida State UniversitySchool of Earth, Ocean and Climate Sciences, Indian Institute of TechnologyIndian Meteorological DepartmentAbstract A new comprehensive surface temperature data set for India is used to document changes in Indian temperature over seven decades, in order to examine the patterns and possible effects of global warming. The data set is subdivided into pre-monsoon, monsoon, and post-monsoon categories in order to study the temperature patterns in each of these periods. When the decade means in maximum, minimum and daily mean temperature for the 2000s are compared to those of the 1950s, a consistent pattern of warming is found over northwestern and southern India, and a pattern of cooling is seen in a broad zone anchored over northeastern India and extending southwestward across central India. These patterns are explained by the presence of a large region of anthropogenic brown haze over India and adjacent ocean regions. These aerosols absorb solar radiation, leading to warming of the haze layer over northeastern and central India and to cooling of the surface air beneath. The heated air rises and then sinks to the north and south of the haze region over northwestern and southern India, warming the air by compression as it sinks in those regions. The possible impact of these temperature patterns on Indian agriculture is considered.https://doi.org/10.1038/s41598-018-25347-2
collection DOAJ
language English
format Article
sources DOAJ
author Robert S. Ross
T. N. Krishnamurti
Sandeep Pattnaik
D. S. Pai
spellingShingle Robert S. Ross
T. N. Krishnamurti
Sandeep Pattnaik
D. S. Pai
Decadal surface temperature trends in India based on a new high-resolution data set
Scientific Reports
author_facet Robert S. Ross
T. N. Krishnamurti
Sandeep Pattnaik
D. S. Pai
author_sort Robert S. Ross
title Decadal surface temperature trends in India based on a new high-resolution data set
title_short Decadal surface temperature trends in India based on a new high-resolution data set
title_full Decadal surface temperature trends in India based on a new high-resolution data set
title_fullStr Decadal surface temperature trends in India based on a new high-resolution data set
title_full_unstemmed Decadal surface temperature trends in India based on a new high-resolution data set
title_sort decadal surface temperature trends in india based on a new high-resolution data set
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2018-05-01
description Abstract A new comprehensive surface temperature data set for India is used to document changes in Indian temperature over seven decades, in order to examine the patterns and possible effects of global warming. The data set is subdivided into pre-monsoon, monsoon, and post-monsoon categories in order to study the temperature patterns in each of these periods. When the decade means in maximum, minimum and daily mean temperature for the 2000s are compared to those of the 1950s, a consistent pattern of warming is found over northwestern and southern India, and a pattern of cooling is seen in a broad zone anchored over northeastern India and extending southwestward across central India. These patterns are explained by the presence of a large region of anthropogenic brown haze over India and adjacent ocean regions. These aerosols absorb solar radiation, leading to warming of the haze layer over northeastern and central India and to cooling of the surface air beneath. The heated air rises and then sinks to the north and south of the haze region over northwestern and southern India, warming the air by compression as it sinks in those regions. The possible impact of these temperature patterns on Indian agriculture is considered.
url https://doi.org/10.1038/s41598-018-25347-2
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