The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District

【Objective】 The increase in atmospheric CO2 and the associated global warming is expected to affect plant growth and development. This paper investigates the spatiotemporal variation in vegetation phenological traits and peak NDVI of plants in Hetao Irrigation District in Inner Mongolia. 【Method】 Th...

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發表在:Guan'gai paishui xuebao
Main Authors: AN Qier, BAO Gang, YUAN Zhihui, WEN Durina, ZHANG Gangdong, CHAO Buga
格式: Article
語言:中文
出版: Science Press 2024-06-01
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在線閱讀:https://www.ggpsxb.com/jgpxxben/ch/reader/view_abstract.aspx?file_no=20240611&flag=1
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author AN Qier
BAO Gang
YUAN Zhihui
WEN Durina
ZHANG Gangdong
CHAO Buga
author_facet AN Qier
BAO Gang
YUAN Zhihui
WEN Durina
ZHANG Gangdong
CHAO Buga
author_sort AN Qier
collection DOAJ
container_title Guan'gai paishui xuebao
description 【Objective】 The increase in atmospheric CO2 and the associated global warming is expected to affect plant growth and development. This paper investigates the spatiotemporal variation in vegetation phenological traits and peak NDVI of plants in Hetao Irrigation District in Inner Mongolia. 【Method】 The analysis was based on MOD13Q1 data from 2001 to 2021. The impact of climatic factors on spatiotemporal variation in the start of season SOS, the end of season (EOS), the length of season (LOS), the peak of season (POS), and the normalized difference vegetation index (NDVI) of the vegetations in the region was analyzed using the two-logistic and four-parameter model. 【Result】 The SOS started from the end of May to the middle of June, and ended from the middle of September to the beginning of October. The annual peak LOS and POS ranged from 95 to 116 days, and from 200 to 220 days, respectively. The annual peak NDVI ranged from 0.5-0.7. Climate change delayed the onset of SOS, reduced LOS, and elevated peak NDVI. Additionally, the delayed SOS contributed to the decrease in LOS. The changes in EOS and POS with climate were consistent. SOS, EOS and POS were negatively correlated to temperature and positively correlated to precipitation. The peak NDVI was positively correlated to temperature and precipitation. 【Conclusion】 The vegetation phenology and peak NDVI in the Hetao Irrigation District were spatially heterogeneous, and the impact of climatic factors on them also varied.
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spelling doaj-art-b8708c8a0b574cbaa7cd2011310e6bca2025-08-20T01:28:13ZzhoScience PressGuan'gai paishui xuebao1672-33172024-06-01436869210.13522/j.cnki.ggps.20234221672-3317(2024)06-0086-07The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation DistrictAN Qier0BAO Gang1YUAN Zhihui2WEN Durina3ZHANG Gangdong4CHAO Buga5(College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China;(College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China;(College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China;(College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China;(College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China;(College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China;【Objective】 The increase in atmospheric CO2 and the associated global warming is expected to affect plant growth and development. This paper investigates the spatiotemporal variation in vegetation phenological traits and peak NDVI of plants in Hetao Irrigation District in Inner Mongolia. 【Method】 The analysis was based on MOD13Q1 data from 2001 to 2021. The impact of climatic factors on spatiotemporal variation in the start of season SOS, the end of season (EOS), the length of season (LOS), the peak of season (POS), and the normalized difference vegetation index (NDVI) of the vegetations in the region was analyzed using the two-logistic and four-parameter model. 【Result】 The SOS started from the end of May to the middle of June, and ended from the middle of September to the beginning of October. The annual peak LOS and POS ranged from 95 to 116 days, and from 200 to 220 days, respectively. The annual peak NDVI ranged from 0.5-0.7. Climate change delayed the onset of SOS, reduced LOS, and elevated peak NDVI. Additionally, the delayed SOS contributed to the decrease in LOS. The changes in EOS and POS with climate were consistent. SOS, EOS and POS were negatively correlated to temperature and positively correlated to precipitation. The peak NDVI was positively correlated to temperature and precipitation. 【Conclusion】 The vegetation phenology and peak NDVI in the Hetao Irrigation District were spatially heterogeneous, and the impact of climatic factors on them also varied.https://www.ggpsxb.com/jgpxxben/ch/reader/view_abstract.aspx?file_no=20240611&flag=1hetao irrigation districtvegetation phenologypeak ndviclimate change
spellingShingle AN Qier
BAO Gang
YUAN Zhihui
WEN Durina
ZHANG Gangdong
CHAO Buga
The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District
hetao irrigation district
vegetation phenology
peak ndvi
climate change
title The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District
title_full The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District
title_fullStr The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District
title_full_unstemmed The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District
title_short The impact of climatic factors on vegetation phenology and peak NDVI in the Hetao Irrigation District
title_sort impact of climatic factors on vegetation phenology and peak ndvi in the hetao irrigation district
topic hetao irrigation district
vegetation phenology
peak ndvi
climate change
url https://www.ggpsxb.com/jgpxxben/ch/reader/view_abstract.aspx?file_no=20240611&flag=1
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