1. 延安大学建筑工程学院,陕西,延安,716000
2. 长安大学旱区地下水文与生态效应教育部重点实验室,西安,710054
3. 长安大学水与环境学院,西安,710054
4. 中国水利水电科学研究院,北京,100038
[ "朱永华(1986-),男,博士,讲师,主要从事生态水文研究。E-mail:zhuyonghua@yau.edu.cn" ]
纸质出版:2022
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ZHU Yonghua, LUO Pingping, GUO Qian, et al. Analysis of Warming and Humidifying Characteristics of Mu Us Sandy Land and Its Influence on Vegetation Change[J]. 2022, 36(5): 160-172.
朱永华, 罗平平, 郭倩, 等. 毛乌素沙地暖湿化特征分析及其对植被变化的影响[J]. 水土保持学报, 2022,36(5):160-172. DOI: 10.13870/j.cnki.stbcxb.2022.05.022.
ZHU Yonghua, LUO Pingping, GUO Qian, et al. Analysis of Warming and Humidifying Characteristics of Mu Us Sandy Land and Its Influence on Vegetation Change[J]. 2022, 36(5): 160-172. DOI: 10.13870/j.cnki.stbcxb.2022.05.022.
气候暖湿化对植被生长及覆盖率乃至土地合理开发利用、生态环境保护均有重要的现实意义。以毛乌素沙地为研究区
基于1959—2019年的气象数据(气温、降水量及蒸发量)
运用气候趋势变化、M-K突变和小波周期分析特征变化
并结合生长季归一化植被指数(normalized difference vegetation index
NDVI)值探究其与研究区气象因子间的响应关系。结果表明:(1)研究区内毛乌素沙地年平均气温、年平均降水量、年平均蒸发量分别升高1.7 ℃、11.19 mm和33.82 mm
并呈显著上升趋势。(2)70年代是气象因子突变始发时间
且在70—90年代间进行了气温由冷变暖、降水由少变多、气候由干变湿的突变。(3)沙地年平均气温、降水及蒸发在时间序列上以20~30年的周期振荡最明显
且在28年处达峰
为毛乌素沙地气象因子变化的第1主周期。(4)1998—2019年NDVI总体呈现波动增加趋势
与蒸发和降水呈正相关的响应关系
蒸发显著性大于降水。研究结果可为当前气候变化下有效保护和管理生态系统提供科学依据。
Climate warming and humidification has important practical significance for vegetation growth and coverage
as well as rational land development and utilization and ecological environment protection. Taking Mu Us sandy land as the study area
based on the meteorological data (temperature
precipitation and evaporation) from 1959 to 2019
this paper analyzed the characteristic changes of climate warming and humidification by using climate trend change
M-K mutation and wavelet cycle
and explored the response relationship between it and meteorological factors in the study area based on normalized difference vegetation index (NDVI) value in the growing season. The results showed that: (1) During the study period
the annual average temperature
annual average precipitation and annual average evaporation in Mu Us sandy land increased by 1.7 ℃
11.19 and 33.82 mm
respectively
and showed a significant upward trend. (2) The 1970s was the starting time of the sudden change of meteorological factors
and the sudden change of temperature from cold to warm
precipitation from less to more
and climate from dry to wet occurred from 1970s to 1990s. (3) The annual average temperature
precipitation and evaporation in the sandy land oscillated most obviously in the period of 20~30 years
and reached the peak at 28 years
which was the first main period of the change of meteorological factors in Mu Us sandy land. (4) From 1998 to 2019
NDVI generally showed a fluctuating and increasing trend
which was positively correlated with evaporation and precipitation. The significance of evaporation was greater than that of precipitation. The research results could provide a scientific basis for the effective protection and management of these valuable ecosystems under the current climate change.
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