Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015

India has experienced extensive land cover and land use change (LCLUC). However, there is still limited empirical research regarding the impact of LCLUC on climate extremes in India. Here, we applied statistical methods to assess how cropland expansion has influenced temperature extremes in India fr...

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Main Authors: Jinxiu Liu, Weihao Shen, Yaqian He
Format: Article
Language:English
Published: MDPI AG 2021-05-01
Series:Land
Subjects:
Online Access:https://www.mdpi.com/2073-445X/10/5/489
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spelling doaj-3d96c00476fb4e12a3bc70825ad9f0ce2021-05-31T23:15:24ZengMDPI AGLand2073-445X2021-05-011048948910.3390/land10050489Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015Jinxiu Liu0Weihao Shen1Yaqian He2School of Information Engineering, China University of Geosciences, Beijing 100083, ChinaSchool of Information Engineering, China University of Geosciences, Beijing 100083, ChinaDepartment of Geography, University of Central Arkansas, Conway, AR 72035, USAIndia has experienced extensive land cover and land use change (LCLUC). However, there is still limited empirical research regarding the impact of LCLUC on climate extremes in India. Here, we applied statistical methods to assess how cropland expansion has influenced temperature extremes in India from 1982 to 2015 using a new land cover and land use dataset and ECMWF Reanalysis V5 (ERA5) climate data. Our results show that during the last 34 years, croplands in western India increased by ~33.7 percentage points. This cropland expansion shows a significantly negative impact on the maxima of daily maximum temperature (TXx), while its impacts on the maxima of daily minimum temperature and the minima of daily maximum and minimum temperature are limited. It is estimated that if cropland expansion had not taken place in western India over the 1982 to 2015 period, TXx would likely have increased by 0.74 (±0.64) °C. The negative impact of croplands on reducing the TXx extreme is likely due to evaporative cooling from intensified evapotranspiration associated with croplands, resulting in increased latent heat flux and decreased sensible heat flux. This study underscores the important influences of cropland expansion on temperature extremes and can be applicable to other geographic regions experiencing LCLUC.https://www.mdpi.com/2073-445X/10/5/489cropland expansionclimate extremeswestern Indianland cover and land use changeGLASS-GLCmaxima of daily maximum temperature
collection DOAJ
language English
format Article
sources DOAJ
author Jinxiu Liu
Weihao Shen
Yaqian He
spellingShingle Jinxiu Liu
Weihao Shen
Yaqian He
Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015
Land
cropland expansion
climate extremes
western Indian
land cover and land use change
GLASS-GLC
maxima of daily maximum temperature
author_facet Jinxiu Liu
Weihao Shen
Yaqian He
author_sort Jinxiu Liu
title Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015
title_short Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015
title_full Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015
title_fullStr Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015
title_full_unstemmed Effects of Cropland Expansion on Temperature Extremes in Western India from 1982 to 2015
title_sort effects of cropland expansion on temperature extremes in western india from 1982 to 2015
publisher MDPI AG
series Land
issn 2073-445X
publishDate 2021-05-01
description India has experienced extensive land cover and land use change (LCLUC). However, there is still limited empirical research regarding the impact of LCLUC on climate extremes in India. Here, we applied statistical methods to assess how cropland expansion has influenced temperature extremes in India from 1982 to 2015 using a new land cover and land use dataset and ECMWF Reanalysis V5 (ERA5) climate data. Our results show that during the last 34 years, croplands in western India increased by ~33.7 percentage points. This cropland expansion shows a significantly negative impact on the maxima of daily maximum temperature (TXx), while its impacts on the maxima of daily minimum temperature and the minima of daily maximum and minimum temperature are limited. It is estimated that if cropland expansion had not taken place in western India over the 1982 to 2015 period, TXx would likely have increased by 0.74 (±0.64) °C. The negative impact of croplands on reducing the TXx extreme is likely due to evaporative cooling from intensified evapotranspiration associated with croplands, resulting in increased latent heat flux and decreased sensible heat flux. This study underscores the important influences of cropland expansion on temperature extremes and can be applicable to other geographic regions experiencing LCLUC.
topic cropland expansion
climate extremes
western Indian
land cover and land use change
GLASS-GLC
maxima of daily maximum temperature
url https://www.mdpi.com/2073-445X/10/5/489
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AT yaqianhe effectsofcroplandexpansionontemperatureextremesinwesternindiafrom1982to2015
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