2014Anhui nongye kexueRequires access

Analysis on Characteristics of Changes in Hot Weather of Mainland China over the Past 57 Years

Cheng Xiao-pin

Open publisher page 0 citations

Abstract

Based on temperature data of 740 stations in China in 1951-2007 and using statistical analysis method,this paper analyzed characteristics of changes in hot weather of mainland China over the past 57 years. Results showed that the change trend is not significant in north China. In the late 1980s,the temperaure rose obviously in north China,while it dropped sharply in southwest areas. In south of the Yangtze River valley,there was no great change after the 1960s and the temperature change was little in Qinghai-Tibet Plateau. In the early period of 1980s,the annual average maximum temperature of China had the lowest change. From then on,there was obvious temperature rise. In addition,change of extreme maximum temperature takes on significant regional difference,and there is high consistency in average change of temperature in south China and north China and regional difference in average maximum temperature. Both gradually rise from north to south. The northeast area is the highest in the difference between the extreme maximum temperature and average maximum temperature and between the extreme maximum temperature and average temperature,followed by northwest area,and the lowest is southwest area. Qinghai-Tibet Plateau is the highest in the difference between average maximum temperature and the average temperature,followed by middle and lower reaches of Yangtze River,and the lowest is south China.

About this research paper

What this paper is about

Based on temperature data of 740 stations in China in 1951-2007 and using statistical analysis method,this paper analyzed characteristics of changes in hot weather of mainland China over the past 57 years. Results showed that the change trend is not significant in north China. In the late 1980s,the temperaure rose obviously in north China,while it dropped sharply in southwest areas. In south of the Yangtze River valley,there was no great change after the 1960s and the temperature change was little in Qinghai-Tibet Plateau. In the early period of 1980s,the annual average maximum temperature of China had the lowest change. From then on,there was obvious temperature rise. In addition,change of extreme maximum temperature takes on significant regional difference,and there is high consistency in average change of temperature in south China and north China and regional difference in average maximum temperature. Both gradually rise from north to south. The northeast area is the highest in the difference between the extreme maximum temperature and average maximum temperature and between the extreme maximum temperature and average temperature,followed by northwest area,and the lowest is southwest area. Qinghai-Tibet Plateau is the highest in the difference between average maximum temperature and the average temperature,followed by middle and lower reaches of Yangtze River,and the lowest is south China.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Based on temperature data of 740 stations in China in 1951-2007 and using statistical analysis method,this paper analyzed characteristics of changes in hot weather of mainland China over the past 57 years. Results showed that the change trend is not significant in north China. In the late 1980s,the temperaure rose obviously in north China,while it dropped sharply in southwest areas. In south of the Yangtze River valley,there was no great change after the 1960s and the temperature change was little in Qinghai-Tibet Plateau. In the early period of 1980s,the annual average maximum temperature of China had the lowest change. From then on,there was obvious temperature rise. In addition,change of extreme maximum temperature takes on significant regional difference,and there is high consistency in average change of temperature in south China and north China and regional difference in average maximum temperature. Both gradually rise from north to south. The northeast area is the highest in the difference between the extreme maximum temperature and average maximum temperature and between the extreme maximum temperature and average temperature,followed by northwest area,and the lowest is southwest area. Qinghai-Tibet Plateau is the highest in the difference between average maximum temperature and the average temperature,followed by middle and lower reaches of Yangtze River,and the lowest is south China.

Key concepts: China, Plateau (mathematics), Climatology, Mainland China, Yangtze river, Mean radiant temperature, Environmental science, Maximum temperature

Related papers

Back to paper searchBrowse research topicsOriginal source
Analysis on Characteristics of Changes in Hot Weather of Mainland China over the Past 57 Years — Research Paper | ScholarLens