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中国区域平均降水量序列构建方法比较研究
引用本文:战云健,任国玉,王朋岭,潘旸,张雷,孙秀宝.中国区域平均降水量序列构建方法比较研究[J].气候与环境研究,2021,26(1):45-57.
作者姓名:战云健  任国玉  王朋岭  潘旸  张雷  孙秀宝
作者单位:国家气象信息中心,北京100081;国家气候中心,北京100081;中国地质大学环境学院大气科学系,武汉430074;国家气候中心,北京100081;中国科学院南海海洋研究所热带海洋环境国家重点实验室,广州510301
基金项目:国家科技基础条件平台专项,国家重点研发计划“全球变化及应对”重点专项2018YFA0605603,2020年中国气象局气候变化专项CCSF202044
摘    要:由于地面观测台站空间分布不均匀,运用不同区域平均技术方法研究中国降水特征和变化规律的结果存在显著差异,是区域降水变化研究不确定性的重要来源之一.本文以"中国地面与CMORPH(CPC Morphing Technique)融合逐日降水产品"作为参照值,基于中国地面2425站观测资料,采用5种网格尺寸的经纬度网格面积加权...

关 键 词:区域平均  降水量  时间序列  气候变化
收稿时间:2020-01-19

Construction Method for Regionally Average Precipitation Time Series in China
Yunjian ZHAN,Guoyu REN,Pengling WANG,Yang PAN,Lei ZHANG,Xiubao SUN.Construction Method for Regionally Average Precipitation Time Series in China[J].Climatic and Environmental Research,2021,26(1):45-57.
Authors:Yunjian ZHAN  Guoyu REN  Pengling WANG  Yang PAN  Lei ZHANG  Xiubao SUN
Institution:1.National Meteorological Information Center, China Meteorological Administration, Beijing 1000812.National Climate Center, China Meteorological Administration, Beijing 1000813.Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 4300744.State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301
Abstract:In China, using different technical methods for studying the regional average precipitation characteristics based on station data could yield significantly different results. In this paper, with "China ground and CMORPH (CPC Morphing Technique) fusion daily precipitation product (V1.0)" as the reference value data, different methods for calculating the regional average precipitation time series in China were compared using the precipitation data of 2425 stations. These methods included the latitude and longitude grid area weighted average method of five grid sizes, the provincial area weighted average method, and the direct average method. The results show that the values of linear trend and the standard deviation of annual precipitation obtained using the 2.5° grid and 5.0° grid area average methods are the closest to those of the reference value. Therefore, 2.5° grid and 5.0° grid area average methods are optimal and suboptimal methods, respectively. The average annual precipitation for 15 years obtained using the provincial area weighted average method, which is commonly used in China’s climate monitoring business, is closest to the reference value. However, its estimation for linear trend and standard deviation is lower than the vale obtained from the 2.5° and 5.0° grid area weighted average methods. The sequence of percentage anomalies is inaccurate. If the grid is too sparse or too dense, the regional average result is far from the reference value. The error in the direct average method is also large, with low reliability.
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