The temperature change of regional difference in Anhui province, China

Ke Liu; Zhiqiang Gao; Wei Gao

doi:10.1117/12.824865

The temperature change of regional difference in Anhui province, China

Ke Liu^*
, Zhiqiang Gao
, Wei Gao

^*Corresponding author for this work

School of Geographic Sciences

East China Normal University
CAS - Institute of Geographical Sciences and Natural Resources Research
Colorado State University

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

Abstract

Three regions, Huaibei, Jianghuai, Jiangnan, are divided based on the topography, climatic characteristics, as well as surface temperature from 1957 to 2006 of 16 stations in Anhui province. The change with the year, season and month is analyzed in Anhui province and three areas. Some conclusions are as follows. Anhui province had the lowest temperature in 1980s, but after that the temperature raised step by step. The warming fastest region is Jianghuai. The same pace of warming is in three areas: the greatest warming in spring, then that in autumn, the last in summer. It is warming remarkable in February and the cooling time occurs in July and December. But the fluctuation in three areas is different in some details. The heat island in Hefei is also researched. It suggests that the urban heat island intensity in 1990s in Hefei was the maximum, and then weakened. At the meanwhile, the summer is cooling and the winter is warming in Hefei.

Original language	English
Title of host publication	Remote Sensing and Modeling of Ecosystems for Sustainability VI
DOIs	https://doi.org/10.1117/12.824865
State	Published - 2009
Event	Remote Sensing and Modeling of Ecosystems for Sustainability VI - San Diego, CA, United States Duration: 5 Aug 2009 → 6 Aug 2009

Publication series

Name	Proceedings of SPIE - The International Society for Optical Engineering
Volume	7454
ISSN (Print)	0277-786X

Conference

Conference	Remote Sensing and Modeling of Ecosystems for Sustainability VI
Country/Territory	United States
City	San Diego, CA
Period	5/08/09 → 6/08/09

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 11 Sustainable Cities and Communities
SDG 13 Climate Action

Keywords

Anhui
Climate change
Urban heat island
Urbanization

Access to Document

10.1117/12.824865

Cite this

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title = "The temperature change of regional difference in Anhui province, China",

abstract = "Three regions, Huaibei, Jianghuai, Jiangnan, are divided based on the topography, climatic characteristics, as well as surface temperature from 1957 to 2006 of 16 stations in Anhui province. The change with the year, season and month is analyzed in Anhui province and three areas. Some conclusions are as follows. Anhui province had the lowest temperature in 1980s, but after that the temperature raised step by step. The warming fastest region is Jianghuai. The same pace of warming is in three areas: the greatest warming in spring, then that in autumn, the last in summer. It is warming remarkable in February and the cooling time occurs in July and December. But the fluctuation in three areas is different in some details. The heat island in Hefei is also researched. It suggests that the urban heat island intensity in 1990s in Hefei was the maximum, and then weakened. At the meanwhile, the summer is cooling and the winter is warming in Hefei.",

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author = "Ke Liu and Zhiqiang Gao and Wei Gao",

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series = "Proceedings of SPIE - The International Society for Optical Engineering",

booktitle = "Remote Sensing and Modeling of Ecosystems for Sustainability VI",

note = "Remote Sensing and Modeling of Ecosystems for Sustainability VI ; Conference date: 05-08-2009 Through 06-08-2009",

}

Liu, K, Gao, Z & Gao, W 2009, The temperature change of regional difference in Anhui province, China. in Remote Sensing and Modeling of Ecosystems for Sustainability VI., 745417, Proceedings of SPIE - The International Society for Optical Engineering, vol. 7454, Remote Sensing and Modeling of Ecosystems for Sustainability VI, San Diego, CA, United States, 5/08/09. https://doi.org/10.1117/12.824865

The temperature change of regional difference in Anhui province, China. / Liu, Ke; Gao, Zhiqiang; Gao, Wei.
Remote Sensing and Modeling of Ecosystems for Sustainability VI. 2009. 745417 (Proceedings of SPIE - The International Society for Optical Engineering; Vol. 7454).

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

TY - GEN

T1 - The temperature change of regional difference in Anhui province, China

AU - Liu, Ke

AU - Gao, Zhiqiang

AU - Gao, Wei

PY - 2009

Y1 - 2009

N2 - Three regions, Huaibei, Jianghuai, Jiangnan, are divided based on the topography, climatic characteristics, as well as surface temperature from 1957 to 2006 of 16 stations in Anhui province. The change with the year, season and month is analyzed in Anhui province and three areas. Some conclusions are as follows. Anhui province had the lowest temperature in 1980s, but after that the temperature raised step by step. The warming fastest region is Jianghuai. The same pace of warming is in three areas: the greatest warming in spring, then that in autumn, the last in summer. It is warming remarkable in February and the cooling time occurs in July and December. But the fluctuation in three areas is different in some details. The heat island in Hefei is also researched. It suggests that the urban heat island intensity in 1990s in Hefei was the maximum, and then weakened. At the meanwhile, the summer is cooling and the winter is warming in Hefei.

AB - Three regions, Huaibei, Jianghuai, Jiangnan, are divided based on the topography, climatic characteristics, as well as surface temperature from 1957 to 2006 of 16 stations in Anhui province. The change with the year, season and month is analyzed in Anhui province and three areas. Some conclusions are as follows. Anhui province had the lowest temperature in 1980s, but after that the temperature raised step by step. The warming fastest region is Jianghuai. The same pace of warming is in three areas: the greatest warming in spring, then that in autumn, the last in summer. It is warming remarkable in February and the cooling time occurs in July and December. But the fluctuation in three areas is different in some details. The heat island in Hefei is also researched. It suggests that the urban heat island intensity in 1990s in Hefei was the maximum, and then weakened. At the meanwhile, the summer is cooling and the winter is warming in Hefei.

KW - Anhui

KW - Climate change

KW - Urban heat island

KW - Urbanization

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SN - 9780819477446

T3 - Proceedings of SPIE - The International Society for Optical Engineering

BT - Remote Sensing and Modeling of Ecosystems for Sustainability VI

T2 - Remote Sensing and Modeling of Ecosystems for Sustainability VI

Y2 - 5 August 2009 through 6 August 2009

ER -

The temperature change of regional difference in Anhui province, China

Abstract

Publication series

Conference

UN SDGs

Keywords

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