欢迎访问《中国农学通报》,

中国农学通报 ›› 2020, Vol. 36 ›› Issue (8): 73-79.doi: 10.11924/j.issn.1000-6850.casb18100091

所属专题: 农业气象

• 资源·环境·生态·土壤·气象 • 上一篇    下一篇

ERA20C资料探究1900—2010年浙江省气温变化

吴昊旻, 姜燕敏   

  1. 丽水市气象局,浙江丽水 323000
  • 收稿日期:2018-10-25 修回日期:2019-01-18 出版日期:2020-03-15 发布日期:2020-03-10
  • 作者简介:吴昊旻,男,1980年出生,浙江丽水人,高级工程师,硕士,研究方向:气候变化及气象网络等。通信地址:323000 浙江省丽水市莲都区寿尔福路85号 丽水市气象局,Tel:0578-2661650,E-mail:wuhaomin8048@163.com。
  • 基金资助:
    丽水市社会科学研究课题"(LC201902);丽水市公益性技术应用研究项目"基于丽水生态优势的气候养生资源区划与应用"(2017GYX51);浙江省气象局科技计划项目"基于GIS的枇杷气候适宜性区划"(2018YB18);丽水市高层次人才项目"枇杷气象灾害监测预警服务技术研究与应用"(2018RC13);丽水市科协服务科技创新项目"丽水市气象旅游景观资源调查"(2018RKT05)

Temperature Changes in Zhejiang from 1900 to 2010 Based on ERA20C

Wu Haomin, Jiang Yanmin   

  1. Lishui Meteorological Bureau, Lishui Zhejiang 323000
  • Received:2018-10-25 Revised:2019-01-18 Online:2020-03-15 Published:2020-03-10

摘要:

利用ERA20C再分析数据集1900—2010年逐月资料,在研究浙江省年际、年代际气温时空分布和年际变率的基础上,检验气温的突变情况,同时细化时间尺度,进一步分析四季气温的时空分布特征,结果显示:浙江省年平均气温16.0℃,增温极为显著,111年来升温0.9℃。地面气温低值区域主要分布在浙江中西部,而高值中心主要出现在沿海地区,气温年际变率最大的地区分布浙江西北部,而变率最小的地方出现在东南沿海一带。Mann-Kendall检验结果显示,1947年气温发生了突变,由缓慢变化转为快速增温。除了冬季之外,浙江省的春、夏、秋3个季节均表现出显著的增温趋势,夏季最为明显,其显著增温趋势为0.13℃/10 a,111年升温1.4℃。春季气温呈现出明显的由东北向西南递增的趋势;夏季的温度变化梯度大,由西南向东北递增,与气候带的纬向分布有较大差别;秋季的气温分布与全年平均较为相似;冬季表现出气温沿海岸线向内陆方向递减(浙江东部)以及由南向北递减(浙江西部)的特点。

关键词: 丽水, 地面气温, 四季, ERA20C

Abstract:

Using the ERA20C monthly reanalysis dataset from 1900 to 2010, inter-annual and inter-decadal variability and spatial and temporal distribution of temperature in Zhejiang Province were analyzed, the mutation of temperature was tested. Then the time scale was refined, the spatial and temporal distribution characteristics of temperature in the four seasons were analyzed. The results showed that the annual average temperature of Zhejiang Province was 16.0℃, significantly increased by 0.9℃ in the past 111 years. Low-value air temperature areas were mainly located in the central and western of Zhejiang, while the high-value areas mainly located in coastal areas. The highest annual temperature variability appeared in the northwestern part of Zhejiang, while the least appeared in the southeastern coastal areas. The Mann-Kendall test showed that there was a mutation in 1947, which was from slow change to rapid warming. Except winter, the spring, summer and autumn showed significant warming trends, especially in summer, with a significant warming trend of 0.13℃/10 a, rising 1.4℃ during the 111 years. The temperature in spring in Zhejiang showed an obvious increasing trend from northeast to southwest. The temperature gradient in summer was large, increased from southwest to northeast, and was quite different from the latitudinal distribution of the climatic zone. The temperature distribution in autumn was similar to the annual average. In winter, the temperature was decreasing along the coastline to the inland (eastern Zhejiang) and decreased from south to north (western Zhejiang).

Key words: Lishui, surface air temperature, the four seasons, ERA20C

中图分类号: