Drivers of Variability in Atmospheric Evaporative Demand: Multiscale Spectral Analysis Based on Observations and Physically Based Modeling. Issue 5 (16th May 2018)

• Record Type: Journal Article
• Authors: Peng, Liqing; Li, Dan; Sheffield, Justin
• Is Part Of: Water resources research. Volume 54:Issue 5(2018)
• Page Start: 3510
• Page End: 3529
• Publication Date: 2018-05-16
• Subjects: potential evapotranspiration -- vapor pressure deficit -- net radiation -- time scale -- dryness; Hydrology -- Periodicals; 333.91
• DOI: 10.1029/2017WR022104
• Languages: English
• ISSNs: 0043-1397

Abstract

Abstract: Atmospheric evaporative demand (AED) is an important variable linking climate with the terrestrial water cycle and the biosphere. Understanding the dynamics of AED has substantial economic, ecological, and social implications. However, how AED varies at different time scales and the drivers of variability remain elusive. This study used spectral coherence analysis to analyze the relationships between observed and modeled AED and climate drivers across multiple time scales at 228 Chinese stations and explored the cross‐scale effects of climate forcings on AED. The results highlight the crucial role of vapor pressure deficit (VPD) in both energy‐limited and water‐limited regions, therefore models that do not incorporate VPD or underestimate the relative importance of VPD have relatively lower skill in predicting AED. Short‐term forcing variability has potential impacts on the long‐term AED changes through temperature and associated land‐atmosphere feedbacks. Our study implies that model predictions for AED and associated hydrologic impacts may not be valid in a changing climate when the key controls on AED and their relative importance are not appropriately represented. Key Points: Spectral coherence analysis revealed drivers of variability in atmospheric evaporative demand across time scales Vapor pressure deficit is essential to predicting atmospheric evaporative demand in both energy‐limited and water‐limited regions The effect of small‐scale forcing variability on atmospheric evaporative demand depends on driver and dryness