Aug 2026· Agriculture· Vol 16, pp. 1662· 1 citation· 128 references
Abstract
Understanding how the spatiotemporal variability of precipitation affects ecosystem respiration (RE) is central to carbon–climate feedback in climate-smart agriculture, yet remains unresolved for the alpine agricultural region of the southern Qinghai–Tibet Plateau, where flux observations are sparse. Using 25 years (2000–2024) of monthly gridded climate and remote sensing data for the Yarlung Zangbo River Basin and Its Two Tributaries Basin, we developed a flux tower-constrained reference–respiration (Rref) environment-matching model in which Rref varies with the enhanced vegetation index (EVI) and land surface temperature (LST) to correct the Lloyd–Taylor parameterization. The correction reduced the RE root mean square error by 54.8% (1.04 → 0.47 gC·m−2·month−1) and eliminated systematic bias (+0.80 → −0.001) relative to an independent gridded RECO product. We then constructed a multidimensional index of precipitation variability (intra-annual concentration, interannual variability, long-term trend, spatial clustering) and combined random forest, spatial regression, lag analysis, and structural equation modeling (SEM) to disentangle direct and indirect pathways from precipitation variability to RE. The central finding is an indirect-conduction mechanism: precipitation concentration (PCI) affects RE almost entirely through vegetation productivity (PCI → GPP → RE, indirect effect −0.676) rather than directly (direct effect +0.076, opposite in sign), because low temperature and high soil water holding capacity buffer the immediate soil moisture response. The basin functions as a net carbon source (mean NEP = −0.550 gC·m−2·month−1) with a significant warming-driven interannual RE increase (Sen’s slope = 0.0025 yr−1, p = 0.022) that is independent of the stable precipitation total. The framework offers a transferable paradigm for carbon flux attribution in alpine regions under sparse observation.
Introduction This study aimed to distinguish drought accumulation timescale from response timing in stable vegetation in the Weihe River Basin. Methods We analyzed MODIS enhanced vegetation index (EVI) and ERA5-Drought standardized precipitation evapotranspiration index (SPEI) data for 2003–2024 on the native 0.25° dro...
Xiang-Xiang Hu, Ya-Ya Shi· Frontiers in Plant Science· 0 citations
Lake area dynamics are sensitive indicators of hydroclimatic variability in cold‐arid regions. We reconstructed lake area changes across the Mongolian Plateau from 1990 to 2025 using Landsat imagery, JRC Global Surface Water, and HydroLAKES, and applied XGBoost and SHAP to examine associations with hydroclimatic, e...
The consequences of tropical forest cover loss for regional hydrometeorology and global ecosystem function represent one of the most pressing environmental challenges of our time. The Yucatán Peninsula (YP) has experienced unprecedented deforestation pressure over recent decades, yet the effects of vegetation loss on p...
N. Gonzalez, David Romero, Gerardo Martín· Earth· 0 citations
Climate change is increasing the frequency and intensity of extreme rainfall events, profoundly affecting vegetation–atmosphere–soil interactions and ecosystem stability. Northeast China (NEC), a major ecological region, is highly sensitive to precipitation variability. However, the annual mechanisms underlying vegetat...