基于源汇指数的沈阳热岛效应

应用生态学报

基于源汇指数的沈阳热岛效应

李丽光¹,许申来²,王宏博¹,赵梓淇¹,蔡福¹,武晋雯¹,陈鹏狮³,张玉书^1**

(¹中国气象局沈阳大气环境研究所, 沈阳 110166; ²北京清控人居环境研究所, 北京 100083; ³辽宁省气象科学研究所, 沈阳 110166)

出版日期:2013-12-18 发布日期:2013-12-18

Urban heat island effect based on urban heat island source and sink indices in Shenyang, Northeast China.

LI Li-guang¹, XU Shen-lai², WANG Hong-bo¹, ZHAO Zi-qi¹, CAI Fu¹, WU Jin-wen¹, CHEN Peng-shi³, ZHANG Yu-shu¹

(¹Institute of Atmospheric Environment, China Meteorological Administration, Shenyang 110166, China; ^2Tsinghua Holdings Human Settlements Environment Institute Co., Ltd, Beijing 100083, China; ³Institute of Meteorological Science, Shenyang 110166, China)

Online:2013-12-18 Published:2013-12-18

摘要/Abstract

摘要： 基于2001和2010年Landsat 遥感影像,利用GIS技术识别沈阳城市热岛源区和汇区,利用地表温度(LST)、源区和汇区面积比率指数（CI）和热岛强度指数（LI）,评价分析了沈阳土地利用发展布局模式对热岛效应的影响.结果表明: 2001—2010年,沈阳三环内土地利用类型变化较大,导致热岛源、汇区面积变化明显,且主要发生在二环和三环.2001年,一环内热岛源、汇区面积比例分别为94.3%和5.7%,三环内分别为64.0%和36.0%;2010年,其比例在一环内分别为93.4%和6.6%,三环内分别为70.2%和29.8%,说明10年来“摊饼式”土地利用布局决定了沈阳热岛效应的“摊饼式”布局.研究期间,沈阳地表温度从一环至三环均呈递减趋势,热岛效应强度在2001年以单一中心为主,至2010年发展为多中心态势,热岛效应强度等级有所降低.从一环至三环,CI绝对值均呈增加趋势,LI值均小于1,说明期间研究区土地利用布局变化对改善区域热岛效应没有明显作用.

Abstract: Based on the remote images in 2001 and 2010, the source and sink areas of urban heat island (UHI) in Shenyang City, Northeast China were determined by GIS technique. The effect of urban regional landscape pattern on UHI effect was assessed with land surface temperature (LST ), area rate index (CI) of the source and sink areas and intensity index (LI) of heat island. The results indicated that the land use type changed significantly from 2001 to 2010, which significantly changed the source and sink areas of UHI, especially in the second and third circle regions. The source and sink areas were 94.3% and 5.7% in the first circle region, 64.0% and 36.0% in the third circle region in 2001, while they were 93.4% and 6.6%, 70.2% and 29.8% in 2010, respectively. It suggested that the land use pattern extended by a round shape in Shenyang led to the corresponding UHI pattern. The LST in the study area tended to decrease from the first circle region to the third. The UHI intensity was characterized with a single center in 2001 and with several centers in 2010, and the grade of UHI intensity was in a decreasing trend from 2001 to 2010. The absolute value of CI increased from the first circle region to the third, and the LI was close to 1, suggesting the change in land use pattern had no significant influence on UHI in Shenyang.

李丽光1,许申来2,王宏博1,赵梓淇1,蔡福1,武晋雯1,陈鹏狮3,张玉书1**. 基于源汇指数的沈阳热岛效应[J]. 应用生态学报.

LI Li-guang1, XU Shen-lai2, WANG Hong-bo1, ZHAO Zi-qi1, CAI Fu1, WU Jin-wen1, CHEN Peng-shi3, ZHANG Yu-shu1. Urban heat island effect based on urban heat island source and sink indices in Shenyang, Northeast China.[J]. Chinese Journal of Applied Ecology.