The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China
Land use and its environmental effects can be quantitatively expressed with land-use intensity. In this study, a land-use intensity metric was improved using a geographic mapping method. The relationships between observed rapid changes in land use and temperature in the Dongting Lake area from 2001...
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Hindawi Limited
2015-01-01
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Series: | Advances in Meteorology |
Online Access: | http://dx.doi.org/10.1155/2015/632151 |
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doaj-39dc416d98604abf91939e0052dc01072020-11-25T01:11:51ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172015-01-01201510.1155/2015/632151632151The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, ChinaWenmin Hu0Weijun Zhou1Hongshi He2College of Resources and Environment, Hunan Agricultural University, Changsha 410128, ChinaCollege of Resources and Environment, Hunan Agricultural University, Changsha 410128, ChinaInstitute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, ChinaLand use and its environmental effects can be quantitatively expressed with land-use intensity. In this study, a land-use intensity metric was improved using a geographic mapping method. The relationships between observed rapid changes in land use and temperature in the Dongting Lake area from 2001 to 2010 were examined. The results revealed the following features: (1) The temperature increased when the land-use intensity increased via a hierarchical transition owing to grass and forest land reductions of 26.25% and 11.74%, respectively; built-up land increased by 48.45%. (2) The temperature increase was driven more by the external environment than by land-use intensity changes. Human activities produced larger effects in the western region than in the eastern or central region of the study area, according to the observed variations in the centres of gravity for temperature and land-use intensity. (3) The temperature response to land-use intensity changes was more sensitive in low-altitude areas than in high-altitude areas; the response presented a north-south gradient, possibly due to socioeconomic and urbanisation differences.http://dx.doi.org/10.1155/2015/632151 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Wenmin Hu Weijun Zhou Hongshi He |
spellingShingle |
Wenmin Hu Weijun Zhou Hongshi He The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China Advances in Meteorology |
author_facet |
Wenmin Hu Weijun Zhou Hongshi He |
author_sort |
Wenmin Hu |
title |
The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China |
title_short |
The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China |
title_full |
The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China |
title_fullStr |
The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China |
title_full_unstemmed |
The Effect of Land-Use Intensity on Surface Temperature in the Dongting Lake Area, China |
title_sort |
effect of land-use intensity on surface temperature in the dongting lake area, china |
publisher |
Hindawi Limited |
series |
Advances in Meteorology |
issn |
1687-9309 1687-9317 |
publishDate |
2015-01-01 |
description |
Land use and its environmental effects can be quantitatively expressed with land-use intensity. In this study, a land-use intensity metric was improved using a geographic mapping method. The relationships between observed rapid changes in land use and temperature in the Dongting Lake area from 2001 to 2010 were examined. The results revealed the following features: (1) The temperature increased when the land-use intensity increased via a hierarchical transition owing to grass and forest land reductions of 26.25% and 11.74%, respectively; built-up land increased by 48.45%. (2) The temperature increase was driven more by the external environment than by land-use intensity changes. Human activities produced larger effects in the western region than in the eastern or central region of the study area, according to the observed variations in the centres of gravity for temperature and land-use intensity. (3) The temperature response to land-use intensity changes was more sensitive in low-altitude areas than in high-altitude areas; the response presented a north-south gradient, possibly due to socioeconomic and urbanisation differences. |
url |
http://dx.doi.org/10.1155/2015/632151 |
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