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基于标准化降水蒸散指数(SPEI)和归一化植被指数(NDVI)的气象干旱响应下植被损失与恢复量化评估框架

An evaluation framework for quantifying vegetation loss and recovery in response to meteorological drought based on SPEI and NDVI.

作者信息

Wu Chuanhao, Zhong Lulu, Yeh Pat J-F, Gong Zhengjie, Lv Wenhan, Chen Bei, Zhou Jun, Li Jiayun, Wang Saisai

机构信息

Yangtze Institute for Conservation and Development, Hohai University, Nanjing 210098, China.

School of Environment, Jinan University, Guangzhou 511436, China.

出版信息

Sci Total Environ. 2024 Jan 1;906:167632. doi: 10.1016/j.scitotenv.2023.167632. Epub 2023 Oct 6.

Abstract

Drought affects vegetation growth to a large extent. Understanding the dynamic changes of vegetation during drought is of great significance for agricultural and ecological management and climate change adaptation. The relations between vegetation and drought have been widely investigated, but how vegetation loss and restoration in response to drought remains unclear. Using the standardized precipitation evapotranspiration index (SPEI) and the normalized difference vegetation index (NDVI) data, this study developed an evaluation framework for exploring the responses of vegetation loss and recovery to meteorological drought, and applied it to the humid subtropical Pearl River basin (PRB) in southern China for estimating the loss and recovery of three vegetation types (forest, grassland, cropland) during drought using the observed NDVI changes. Results indicate that vegetation is more sensitive to drought in high-elevation areas (lag time < 3 months) than that in low-elevation areas (lag time > 8 months). Vegetation loss (especially in cropland) is found to be more sensitive to drought duration than drought severity and peak. No obvious linear relationship between drought intensity and the extent of vegetation loss is found. Regardless of the intensity, drought can cause the largest probability of mild loss of vegetation, followed by moderate loss, and the least probability of severe loss. Large spatial variability in the probability of vegetation loss and recovery time is found over the study domain, with a higher probability (up to 50 %) of drought-induced vegetation loss and a longer recovery time (>7 months) mostly in the high-elevation areas. Further analysis suggests that forest shows higher but cropland shows lower drought resistance than other vegetation types, and grassland requires a shorter recovery time (4.2-month) after loss than forest (5.1-month) and cropland (4.8-month).

摘要

干旱在很大程度上影响植被生长。了解干旱期间植被的动态变化对于农业和生态管理以及适应气候变化具有重要意义。植被与干旱之间的关系已得到广泛研究,但植被如何响应干旱而损失和恢复仍不清楚。本研究利用标准化降水蒸散指数(SPEI)和归一化植被指数(NDVI)数据,建立了一个评估框架,以探讨植被损失和恢复对气象干旱的响应,并将其应用于中国南方湿润亚热带珠江流域(PRB),利用观测到的NDVI变化估算干旱期间三种植被类型(森林、草地、农田)的损失和恢复情况。结果表明,高海拔地区(滞后时间<3个月)的植被比低海拔地区(滞后时间>8个月)的植被对干旱更敏感。发现植被损失(尤其是农田)对干旱持续时间比对干旱严重程度和峰值更敏感。未发现干旱强度与植被损失程度之间存在明显的线性关系。无论强度如何,干旱导致植被轻度损失的概率最大,其次是中度损失,重度损失的概率最小。研究区域内植被损失概率和恢复时间存在较大的空间变异性,干旱导致植被损失的概率较高(高达50%),恢复时间较长(>7个月),主要集中在高海拔地区。进一步分析表明,森林的抗旱性高于其他植被类型,而农田的抗旱性低于其他植被类型,草地损失后的恢复时间(4.2个月)比森林(5.1个月)和农田(4.8个月)短。

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