摘要
气候舒适度对人类活动和地区适宜性评价等研究具有重要意义,而温湿指数是气候舒适度评价的一项重要指标。传统的温湿指数计算都是基于站点数据,无法获取大尺度区域舒适度的时空变化特征。本文利用2005—2018年MODIS地表温度、大气可降水量数据,结合地理加权回归方法对经典温湿指数模型进行改进,计算并分析中国年均和月均气候舒适度时空演变特征。结果如下:①采用GWR方法进行地表温度和气温的拟合,拟合精度(Adjusted R^2=0.9~0.98,RMSE=0.14~1.89℃)较为理想,说明采用LST、NDVI、DEM作为自变量的地理加权回归分析,能够较精确地拟合地面气温;②2005—2018年年均温湿指数统计结果表示,云南省累计舒适月数最多,高达167个月,中部省份相对于东南沿海省市舒适时期较多,最高舒适月数差值可达到41个月。中国年均舒适度空间分布规律基本保持一致,除新疆、西藏和东北的部分区域以外,舒适度空间呈现从南到北,舒适度等级由舒适变寒冷。从舒适度等级面积变化情况看,2005—2018年全国舒适度等级呈现由寒冷变舒适的趋势;③2018年全年舒适面积最大的月份为5月,其次为10月,不舒适月份集中在1月和7月,全国呈现极冷或极热。春季和秋季空间分布特征较为相似,呈现由东南到西北逐渐递减的趋势;除青藏高原地区外,夏季和冬季呈现由南到北递减趋势。舒适区域主要集中在低纬、中海拔地区。
Climate comfort level has great significance to human activities and regional suitability assessment,and temperature humidity index is important for climate comfort evaluation.Traditional temperature-humidity index is obtained based on the observed data from some sations,which cannot reflect the spatio-temporal characteristics of climate comfort in large-scale areas.In this paper,the modified temperature humidity index model is proposed using Land Surface Temperature(LST)and Precipitable Water Vapor(PWV)from 2005 to 2018 retrieved from MODIS.Using this new index,the spatio-temporal characteristics of climate comfort level in China are calculated and analyzed.The results are shown as follows:(1)The GWR method is used to fit the surface temperature and air temperature.The fitting accuracy(Adjusted R2=0.90~0.98,RMSE=0.14~1.89℃)is ideal,which indicates that LST,NDVI,and DEM are used as the independent variables for geographical weight Regression analysis can more accurately fit the air temperature;(2)The statistical results of the annual average temperature and humidity index from 2005 to 2018 show that the cumulative number of comfortable months in Yunnan Province is the most,up to 167 months,and the central provinces are relatively comfortable compared to the southeast coastal provinces,and the difference between the highest comfort months can reach 41 months.The spatial distribution of China’s average annual comfort level is basically the same.Except for parts of Xinjiang,Tibet,and the northeast,the comfort level in China is from south to north,and the comfort level changes from comfortable to cold.Judging from the changes in the area of each comfort level,the national comfort level showed a trend from cold to comfortable from 2005 to 2018;(3)The month with largest comfortable area in 2018 is May,followed by October.Uncomfortable months are concentrated in January and July when the country is extremely cold or hot.The spatial distribution characteristics of spring and autumn are similar,showing a gradual decreasing trend from southeast to northwest;except for the Qinghai-Tibet Plateau,summer and winter show a decreasing trend from south to north.The comfort zone is mainly concentrated in low-latitude and middle-altitude areas.
作者
刘艳霞
冯莉
田慧慧
阳少奇
LIU Yanxia;FENG Li;TIAN Huihui;YANG Shaoqi(School of Hydrology and Water Resources,Hohai University,Nanjing 211100,China)
出处
《地球信息科学学报》
CSCD
北大核心
2020年第12期2338-2347,共10页
Journal of Geo-information Science
基金
国家自然科学基金项目(41771446)
中央高校基本科研业务费项目(2018B18414)。
关键词
气候舒适度
时空分布特征
温湿指数
地理加权回归
地表温度
大气可降水量
MODIS
中国
climate comfort level
spatiotemporal distribution
temperature-humidity index
geographically weighted regression
land surface temperature
precipitable water vapor
MODIS
China
