首页|黄河中游晋西黄土高原近62年气候变化分析

黄河中游晋西黄土高原近62年气候变化分析

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通过对9个地面站的年平均气温和年平均降水量数据进行分析,研究了黄河中游晋西黄土高原近62 a(1957年至2018年)的气候变化情况.结果表明,1957年至2018年,黄河中游晋西黄土高原气温显著升高,年平均增温0.0230 ℃.其中,北部区域和中部区域年平均增温为0.0288℃和0.0354℃,线性方程达到极显著水平;南部区域年平均增温0.0176℃,线性方程达到显著水平,增温趋势相对平缓.全区年平均降水量减少0.324 mm,线性方程未达到显著水平,从北向南降水量减少量增加.总体来看,区域气候环境总体趋于暖干化.
Climate Change of the Western Shanxi Loess Plateau in the Middle Reaches of Yellow River over the Last 62 Years
By analyzing the annual average temperature and precipitation data from 9 ground stations,the climate change in the western Shanxi Loess Plateau in the middle reaches of the Yellow River over the past 62 years(1957 to 2018)was stud-ied.The results showed that from 1957 to 2018,the temperature of the western Shanxi Loess Plateau in the middle reaches of the Yellow River significantly increased,with an average annual temperature increase of 0.023 0 ℃.Among them,the annual average temperature increase in the northern region and central region were 0.028 8 ℃ and 0.035 4 ℃,and the line-ar equation reached a highly significant level.The annual average temperature increase in the southern region was 0.017 6 ℃with a relatively gentle warming trend,which linear equation reached a significant level.The annual average precipitation in the entire region decreased by 0.324 mm,and the linear equation did not reach a significant level.The decrease in precipi-tation increased from north to south.Overall,the regional climate environment presented a warm and dry trend.

Western Shanxi Loess Plateau in the middle reaches of Yellow RiverAverage annual temperatureAnnual av-erage precipitationVariation trend

张晓玲、马佳琳、李新平

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山西省林业和草原科学研究院,山西 太原 030012

亚洲开发银行知识和技术援助项目咨询顾问,山西 太原 030012

黄河中游晋西黄土高原 年平均气温 年平均降水量 变化趋势

亚洲开发银行(ADB)知识和技术支持援助(TA)集群项目

54026-012

2024

山西林业科技
山西省林业科学研究院,山西省林学会

山西林业科技

影响因子:0.259
ISSN:1007-726X
年,卷(期):2024.53(1)
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