2015―2016年塔克拉玛干沙漠腹地天然绿洲气温及相对湿度变化特征

黄晶晶; 张峰; 师庆东; 金莉莉

doi:10.13568/j.cnki.651094.2019.03.003

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2015―2016年塔克拉玛干沙漠腹地天然绿洲气温及相对湿度变化特征

专栏:绿洲生态学 | 更新时间：2026-01-21

- 2015―2016年塔克拉玛干沙漠腹地天然绿洲气温及相对湿度变化特征
- 2015―2016年塔克拉玛干沙漠腹地天然绿洲气温及相对湿度变化特征
- 新疆大学学报（自然科学版中英文） 2019年36卷第3期页码：267-275
- 作者机构：
  
  1. 新疆大学绿洲生态教育部重点实验室
  2. 中国气象局乌鲁木齐沙漠气象研究所塔克拉玛干沙漠大气环境观测试验站
- 作者简介：
- 基金信息：
  
  国家自然科学基金新疆联合基金项目(U1178303;U1703237)
- DOI：10.13568/j.cnki.651094.2019.03.003
  中图分类号： P423;P426.1
- 纸质出版：2019
- 稿件说明：
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[1]黄晶晶,张峰,师庆东,等.2015―2016年塔克拉玛干沙漠腹地天然绿洲气温及相对湿度变化特征[J].新疆大学学报(自然科学版),2019,36(03):267-275.
[1]黄晶晶,张峰,师庆东,等.2015―2016年塔克拉玛干沙漠腹地天然绿洲气温及相对湿度变化特征[J].新疆大学学报(自然科学版),2019,36(03):267-275. DOI： 10.13568/j.cnki.651094.2019.03.003.

DOI：10.13568/j.cnki.651094.2019.03.003.

摘要

达理雅博依绿洲是塔克拉玛干沙漠腹地现存最大的一处天然绿洲

其气象参数的获取可为干旱区绿洲生态环境及绿洲的形成及演变等问题的研究提供基础数据.本文分析了2015―2016年在达理雅博依所设置的首台区域气象站气温及相对湿度变化特征.结果表明:2015年绿洲平均气温值为11.8℃

气温日变化较急剧;年内月均气温最高值出现在7月

为28.6℃

最低值出现在1月

为-6.7℃;绿洲平均相对湿度为40.2%;年内月均相对湿度最高值出现在12月

为60.3%

最低值出现在4月

为25.6%;呈现典型的暖温带大陆性气候特征.与处于同纬度的沙漠腹地相比

绿洲月均气温最高值比塔中地区低1.4℃

最低值则高1.5℃

月均相对湿度最高值低2.7%

最低值高4.6%

显示出天然绿洲与沙漠环境的差异;相比位于上游的人工绿洲

其月均气温最高值比于田县要高1.8℃

最低值低4℃

月均相对湿度最高值高5.3%

最低值较3月于田县的23.0%低2.6%

显示沙漠环境对其腹地绿洲的影响要较其边缘人工绿洲大.

Abstract

Daliyaboyi is the largest natural oasis in the hinterland of the Taklamakan Desert

measuring the natural oasis' meteorological parameters will provide fundamental data for the study of ecological environment and the formation and evolution of oases in arid regions. We analyzed the characteristics of temperature and relative humidity data(2015―2016) from the first regional meteorological station set up at Daliyaboyi. The results showed that the average temperature of the oasis was 11.8 ℃ in 2015

where the daily temperature varied rapidly. The highest temperature of 2015

which appeared in July

was 28.6 ℃

and the lowest

which was in January

was-6.7℃. The average relative humidity of Daliyaboyi was 40.2% in 2015

and its highest monthly average relative humi-dity was 60.3%

which was in December

and the lowest

which was in April

was 25.6%. This presents a warm temperate climate type continental climate. Compared to Tazhong station

which is located at a similar latitude and in the desert hinterland

the highest temperature over the year at Daliyaboyi was 1.4 ℃ lower than that at Tazhong and its lowest temperature was 1.5 ℃ higher than that of Tazhong

the highest monthly average relative humidity was 2.7% lower than that at Tazhong and its lowest monthly average relative humidity was 4.6% higher than that of Tazhong

this suggests that there is a difference between a natural oasis and the desert environment.However

compared to Yutian

which is an artificial oasis in the upper stream and the southern margin of the Tarim Basin

the highest temperature value in Daliyaboyi was 1.8 ℃ higher than that at Yutian and the lowest value was 4 ℃ lower than that at Yutian

the highest monthly average relative humidity was 5.3% higher than that at Yutian and its lowest monthly average relative humidity was 2.6% lower than that of Yutian in March(23.0%)

which indicated the impact of the desert on its hinterland oasis was greater than on its edges.

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