دورية أكاديمية

Quantifying the impact of climate and vegetation changes on runoff based on the budyko framework in the Lake Issyk-Kul Basin, Kyrgyzstan

التفاصيل البيبلوغرافية
العنوان: Quantifying the impact of climate and vegetation changes on runoff based on the budyko framework in the Lake Issyk-Kul Basin, Kyrgyzstan
المؤلفون: Pingping Feng, Yilinuer Alifujiang, Jilili Abuduwaili, Na Lu, Ying Jiang
المصدر: Frontiers in Earth Science, Vol 11 (2023)
بيانات النشر: Frontiers Media S.A., 2023.
سنة النشر: 2023
المجموعة: LCC:Science
مصطلحات موضوعية: budyko model, runoff, climate factors, vegetation, NDVI, Lake Issyk-Kul Basin, Science
الوصف: Identifying and quantifying the drivers of runoff (R) variability is fundamental to our understanding of the hydrologic cycle and necessary for decision makers to manage water resources. Climate variables and vegetation are the main factors influencing the R. However, the effects of climate and vegetation changes on R are still poorly understood, especially in arid regions with limited water resources. This study quantifies the contribution of precipitation (PRE), potential evapotranspiration (ET0), and Normalized Difference Vegetation Index (NDVI) to R in Lake Issyk-Kul Basin (LIKB) dryland Central Asia by using the Budyko model. The results showed that R, PRE, and ET0 decreased from 2000 to 2020, while the NDVI and underlying parameter (ω) showed a slightly increasing trend. By using the Mann-Kendall (M-K) statistical approach, divided the R series into a baseline period (2000–2010) and a change period (2011–2020) based on the breakthrough point (2011). In the baseline period, R showed a decreasing trend, while in the change period, R showed an increasing trend of 1.8 mm/yr. The sensitivity analysis shows that a 1 mm increase in PRE results in a 0.48 mm increase in R (sensitivity coefficient to R is 0.48). Conversely, a 1 mm increase in ET0 (sensitivity coefficient to R of −0.03) and a 1 unit increase in NDVI (sensitivity coefficient to R of −343.31) lead to R decreasing by 0.03 and 343.31 mm, respectively. The relative contributions of PRE, ET0 and NDVI were 33.98%, −3.17% and 3.67%, respectively, suggesting that changes in PRE and NDVI contributed to the decrease in R while the opposite for ET0. PRE dominated the decrease in R, which decreased by 26.58 mm, leading to a decrease in R of 12.76 mm. A decrease of 65.33 mm in ET0 and an increase of 0.003 in NDVI resulted in an increase and decrease of 1.96 and 1.18 mm in R, respectively. This study enhances the understanding of the response of the water cycle to climate and vegetation changes in arid regions and can provide theoretical support for water resource management and ecological restoration.
نوع الوثيقة: article
وصف الملف: electronic resource
اللغة: English
تدمد: 2296-6463
Relation: https://www.frontiersin.org/articles/10.3389/feart.2023.1251759/full; https://doaj.org/toc/2296-6463
DOI: 10.3389/feart.2023.1251759
URL الوصول: https://doaj.org/article/ce09a8e75b284877bb0965b268ee2851
رقم الأكسشن: edsdoj.09a8e75b284877bb0965b268ee2851
قاعدة البيانات: Directory of Open Access Journals
الوصف
تدمد:22966463
DOI:10.3389/feart.2023.1251759