Analysis on Characteristics of Vegetation Evolution and Its Impact on Sandstorm in Shiyang River Basin Based on NDVI

LUO Xiaoling; YANG Mei; LI Yanying; JIANG Jufang; NIE Xin

doi:10.13870/j.cnki.stbcxb.2022.02.011

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Analysis on Characteristics of Vegetation Evolution and Its Impact on Sandstorm in Shiyang River Basin Based on NDVI

更新时间：2024-11-07

- Analysis on Characteristics of Vegetation Evolution and Its Impact on Sandstorm in Shiyang River Basin Based on NDVI
- Vol. 36, Issue 2, Pages: 84-91(2022)
- 作者机构：
  
  1. 甘肃省武威市气象局,甘肃,武威,733000
  2. 中国气象局兰州干旱气象研究所, 甘肃省干旱气候变化与减灾重点实验室, 中国气象局干旱气候变化与减灾重点开放实验室,兰州,730020
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2022.02.011
  CLC： P445
- Published：2022
- 稿件说明：
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LUO Xiaoling, YANG Mei, LI Yanying, et al. Analysis on Characteristics of Vegetation Evolution and Its Impact on Sandstorm in Shiyang River Basin Based on NDVI[J]. 2022, 36(2): 84-91.
DOI：

LUO Xiaoling, YANG Mei, LI Yanying, et al. Analysis on Characteristics of Vegetation Evolution and Its Impact on Sandstorm in Shiyang River Basin Based on NDVI[J]. 2022, 36(2): 84-91. DOI： 10.13870/j.cnki.stbcxb.2022.02.011.

摘要

利用石羊河流域2000-2016年卫星遥感数据和7个气象站1961-2020年逐日沙尘暴资料

使用一元回归趋势法、线性倾向率、相关系数等方法

分析该流域植被覆盖与沙尘暴频次、持续时间、强度的多尺度变化特征及关系

探讨其对沙尘暴发生发展的影响程度。结果表明:流域植被轻微增大

NDVI以每年0.0009的速度增大

2007年开始恢复

2010年以后恢复比较明显

上中游恢复速度比下游快。沙尘暴频次显著减少

年际倾向率为-2.8 d/10 a

近10年减少最显著

较70年代减少14.5天;中游减少速度较慢

下游减少速度较快;四季减少速度为春季>夏季>冬季>秋季。沙尘暴持续时间显著缩短

年际倾向率为-12.2 m/10 a

近10年持续时间最短

较70年代缩短了60.9 min;中游缩短时间较慢

下游缩短时间较快。沙尘暴强度无明显变化

最小能见度维持在0.496 km左右。沙尘暴频次和持续时间与当年和前1年全流域NDVI、NDVI>0.3面积、上中下游NDVI呈显著负相关。沙尘暴强度与当年全流域NDVI、NDVI>0.3面积、上中下游NDVI呈弱负相关

与前1年的NDVI因子呈弱正相关。流域植被覆盖的改善对沙尘暴有明显抑制作用。

Abstract

Based on the satellite remote sensing data from 2000 to 2020 and the daily sandstorm data of seven meteorological stations from 1961 to 2020 in the Shiyang River Basin

we analyzed the multi-scale variation characteristics and relationship between watershed vegetation coverage and sandstorm frequency

duration and intensity

and explored its influence on the occurrence and development of sandstorm by using the methods of univariate regression trend method

linear tendency rate and correlation coefficient. The results showed that the watershed vegetation coverage increased slightly

and NDVI increased at the rate of 0.000 9 per year. The NDVI began to recover in 2007. Recovery was more obvious after 2010

and the recovery rates in the upper and middle reaches were faster than that in the lower reaches. The sandstorm frequency decreased significantly

and the interannual trend rate was -2.8 d/10 a. It decreased the most significantly in the past 10 years

which was 14.5 days less than that in the 1970s. The rate of reduction was slower in the middle reaches and that was faster in the lower reaches. The rate of reduction in four seasons followed the order of spring>summer>winter>autumn. The sandstorm duration was significantly shortened

the interannual trend rate was -12.2 m/10 a. The duration in the last 10 years was the shortest

which was 60.9 min shorter than that in the 1970s. The shorting time in the middle reaches was slower and that was faster in the lower reaches. The sandstorm intensity had no obvious change

and the minimum visibility was around 0.496 km. The frequency and duration of sandstorm were negatively correlated with full-basin NDVI

NDVI >0.3 area

NDVI of upper

middle and lower reaches in the current year and the previous year. The sandstorm intensity had a weak negative correlation with full-basin NDVI

NDVI >0.3 area

NDVI of upper

middle and lower reaches

and a weak positive correlation with NDVI of the previous year. The improvement of vegetation cover in the watershed had obvious restraining effect on sandstorm.

关键词

Keywords

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