| 植被覆盖状况影响中国地表气温变化的观测事实 |
| |
| 引用本文： | 杨续超,张镱锂,丁明军,刘林山,王兆锋,高大伟.植被覆盖状况影响中国地表气温变化的观测事实[J].地球物理学报,2010,53(4):833-841. |
| |
| 作者姓名： | 杨续超 张镱锂 丁明军 刘林山 王兆锋 高大伟 |
| |
| 作者单位： | 1.浙江省气象科学研究所， 杭州 310017;2.中国科学院地理科学与资源研究所，北京 100101;3.江西师范大学地理与环境学院，南昌 330022;4.浙江省气候中心， 杭州 310017 |
| |
| 基金项目： | 国家重点基础研究发展计划(2005CB422006)、国家自然科学基金（40771206、40675057）、中国气象局气候变化专项（CCSF-09-10）资助. |
| |
| 摘 要： | 利用NOAA/AVHRR归一化植被指数（NDVI）及观测气温与再分析地表气温的差值（Observation Minus Reanalysis, OMR）分析了植被覆盖状况对中国地表气温变化的影响.结果表明，地表气温OMR趋势值与NDVI在空间上呈现出显著的负相关关系，植被覆盖状况差（NDVI小于0.1）的区域地表升温较为显著，气温OMR趋势值超过0.2℃/10a，而植被覆盖度高（NDVI大于0.5）的区域气温OMR趋势值则变化不大，甚至出现降温.气温OMR趋势值对植被的季节变化还有着敏感的响应.不同区域植被覆盖状况的差异可能导致中国地表气温变化对全球变暖的响应不同，预测中国未来气候变化需要考虑植被覆盖状况及其动态变化的影响.
|
| 关 键 词： | 地表气温 NDVI OMR方法 观测资料 再分析资料 |
| 收稿时间： | 2009-06-19 |
| 修稿时间： | 2010-02-22 |
Observational evidence of the impact of vegetation cover on surface air temperature change in China |
| |
| YANG Xu-Chao,ZHANG Yi-Li,DING Meng-Jun,LIU Lin-Shan,WANG Zhao-Feng,GAO Da-Wei.Observational evidence of the impact of vegetation cover on surface air temperature change in China[J].Chinese Journal of Geophysics,2010,53(4):833-841. |
| |
| Authors: | YANG Xu-Chao ZHANG Yi-Li DING Meng-Jun LIU Lin-Shan WANG Zhao-Feng GAO Da-Wei |
| |
| Institution: | 1.Institute of Meteorology, Zhejiang Metelrological Bureau, Hangzhou 310017, China;2.Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences，Beijing 100101, China;3.School of Geography and Environment, Jiangxi Normal University, Nanchang 330022, China;4.Climate Center of Zhejiang Province, Hangzhou 310017, China |
| |
| Abstract: | Using NOAA/AVHRR normalized difference vegetation index (NDVI) data, the impact of vegetation cover on surface air temperature change is investigated by subtracting the reanalysis from the observation (observation minus reanalysis, OMR). The results show that the temperature OMR trend is inversely correlated to the surface vegetation index and the strong (weak) surface warming corresponds to the surface barrenness (greenness). Areas with NDVI less than 0.1 show a large warming trend of more than 0.2℃/10a, but areas with NDVI larger than 0.5 show little surface warming and even decreasing trends of temperature. Moreover, the OMR trend sensitively responds to the seasonal vegetation cover change. Atmosphere-land feedbacks over areas with different vegetation covers can alter the response of regional surface air temperature to global warming induced by the increase in anthropogenic greenhouse gases concentrations. Thus, it is suggested that projection of future surface climate of China should incorporate the impacts of spatio-temporal variability in vegetation cover. |
| |
| Keywords: | Surface air temperature NDVI OMR method Observations Reanalysis |
| 本文献已被 万方数据 等数据库收录！ |
| 点击此处可从《地球物理学报》浏览原始摘要信息 |
| 点击此处可从《地球物理学报》下载免费的PDF全文 |
|
