Quantifying the role of soil in local precipitation redistribution to vegetation growth

Precipitation is the primary source of water available to vegetation. Although many studies have explored the spatially heterogeneous relationship between vegetation and precipitation, it remains unknown why different precipitation levels lead to comparable vegetation growth and the same precipitati...

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Main Authors: Xinrong Zhu, Hongyan Liu, Yunyun Li, Boyi Liang
Format: Article
Language:English
Published: Elsevier 2021-05-01
Series:Ecological Indicators
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1470160X21000200
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author Xinrong Zhu
Hongyan Liu
Yunyun Li
Boyi Liang
author_facet Xinrong Zhu
Hongyan Liu
Yunyun Li
Boyi Liang
author_sort Xinrong Zhu
collection DOAJ
description Precipitation is the primary source of water available to vegetation. Although many studies have explored the spatially heterogeneous relationship between vegetation and precipitation, it remains unknown why different precipitation levels lead to comparable vegetation growth and the same precipitation level leads to different vegetation growth. Here we provided a simple, new parameterized calculation method to describe the precipitation-vegetation relation. The new method characterizes the ability of local precipitation to supply the water needed for vegetation growth. In the case of China, the method can explain vegetation growth better than the common indices that represent water supply, such as the SPEI, the PDSI, and soil moisture. We further explored what induces the differences in the capacity of soil to redistribute local precipitation for vegetation growth by examining the sensitivity of the residual value between actual vegetation growth and theoretical precipitation-determined vegetation growth to water storage-related soil properties. Our results indicate that soil texture and soil depth to bedrock rather than climatic factors predicted the above mentioned residual values, which implies that soil water storage capacity can increase or decrease the amount of local precipitation needed for vegetation growth. Soil physical properties that involve a high clay content and a thickness between 1 and 3 m are favorable for the stored precipitation fraction for vegetation growth. Neglecting this effect of soil water storage capacity may introduce inaccuracies when simulating the impact of future climate change on vegetation growth.
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spelling doaj.art-6e3e0187e8ca4083b97b4c5d81599e7b2022-12-21T19:09:39ZengElsevierEcological Indicators1470-160X2021-05-01124107355Quantifying the role of soil in local precipitation redistribution to vegetation growthXinrong Zhu0Hongyan Liu1Yunyun Li2Boyi Liang3College of Urban and Environment Sciences and MOE Laboratory for Earth Surface Processes, Peking University, Beijing 100871, ChinaCollege of Urban and Environment Sciences and MOE Laboratory for Earth Surface Processes, Peking University, Beijing 100871, China; Corresponding author.College of Urban and Environment Sciences and MOE Laboratory for Earth Surface Processes, Peking University, Beijing 100871, ChinaCollege of Urban and Environment Sciences and MOE Laboratory for Earth Surface Processes, Peking University, Beijing 100871, China; Geography, College of Life and Environmental Sciences, Amory Building, University of Exeter, Rennes Drive, Exeter EX4 4QD, UKPrecipitation is the primary source of water available to vegetation. Although many studies have explored the spatially heterogeneous relationship between vegetation and precipitation, it remains unknown why different precipitation levels lead to comparable vegetation growth and the same precipitation level leads to different vegetation growth. Here we provided a simple, new parameterized calculation method to describe the precipitation-vegetation relation. The new method characterizes the ability of local precipitation to supply the water needed for vegetation growth. In the case of China, the method can explain vegetation growth better than the common indices that represent water supply, such as the SPEI, the PDSI, and soil moisture. We further explored what induces the differences in the capacity of soil to redistribute local precipitation for vegetation growth by examining the sensitivity of the residual value between actual vegetation growth and theoretical precipitation-determined vegetation growth to water storage-related soil properties. Our results indicate that soil texture and soil depth to bedrock rather than climatic factors predicted the above mentioned residual values, which implies that soil water storage capacity can increase or decrease the amount of local precipitation needed for vegetation growth. Soil physical properties that involve a high clay content and a thickness between 1 and 3 m are favorable for the stored precipitation fraction for vegetation growth. Neglecting this effect of soil water storage capacity may introduce inaccuracies when simulating the impact of future climate change on vegetation growth.http://www.sciencedirect.com/science/article/pii/S1470160X21000200Precipitation supply sufficiencyPrecipitation vegetation drought index (PVDI)Vegetation growthSoil water storage
spellingShingle Xinrong Zhu
Hongyan Liu
Yunyun Li
Boyi Liang
Quantifying the role of soil in local precipitation redistribution to vegetation growth
Ecological Indicators
Precipitation supply sufficiency
Precipitation vegetation drought index (PVDI)
Vegetation growth
Soil water storage
title Quantifying the role of soil in local precipitation redistribution to vegetation growth
title_full Quantifying the role of soil in local precipitation redistribution to vegetation growth
title_fullStr Quantifying the role of soil in local precipitation redistribution to vegetation growth
title_full_unstemmed Quantifying the role of soil in local precipitation redistribution to vegetation growth
title_short Quantifying the role of soil in local precipitation redistribution to vegetation growth
title_sort quantifying the role of soil in local precipitation redistribution to vegetation growth
topic Precipitation supply sufficiency
Precipitation vegetation drought index (PVDI)
Vegetation growth
Soil water storage
url http://www.sciencedirect.com/science/article/pii/S1470160X21000200
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AT yunyunli quantifyingtheroleofsoilinlocalprecipitationredistributiontovegetationgrowth
AT boyiliang quantifyingtheroleofsoilinlocalprecipitationredistributiontovegetationgrowth