Hysteresis in seasonal land-atmospheric interactions over India and its characteristics across croplands and forests

• Published in: Environmental research letters 2024-12, Vol.19 (12), p.124043
• Main Authors: Khandare, Ajinkya, Murtugudde, Raghu, Karthikeyan, L, Ghosh, Subimal
• Format: Article
• Language: English
• Subjects: Agricultural land; Capacitors; Evaporation; Evapotranspiration; Forests; Hydrologic models; Hysteresis; land-atmosphere interaction; Moisture content; Monsoons; Optical analysis; Optical thickness; Parameterization; Precipitation; Productivity; Rain water; Soil dynamics; Soil moisture; Soil profiles; Soil properties; Soil water; Soil water storage; soil-vegetation continuum; terrestrial ecosystem productivity; Vegetation; Wind
• ISSN: 1748-9326; 1748-9326
• DOI: 10.1088/1748-9326/ad893e

Satellite-derived vegetation optical depth and soil moisture (SM) data reveal the critical role of the soil-vegetation continuum in storing rainwater during the Indian Summer Monsoon and supporting evapotranspiration (ET) during the dry non-monsoon season. During the non-monsoon drier period, the climatologically estimated spatial mean of ET exceeds precipitation input, a phenomenon known as the soil–vegetation capacitor effect, which is pivotal in maintaining ecosystem productivity. Notably, our analysis reveals significant variations in the capacitor period between croplands and forests, with croplands exhibiting a ∼77 d longer due to dual crop seasons influenced by regional precipitation. The well-recognized hysteresis curves, observed in magnetization and soil–water characteristic curves, highlight phenomena where a system’s state is influenced by its historical inputs or states and are integral to our findings. We report a previously undocumented seasonal hysteresis in the relationship between the evaporative fraction (EVF) and SM for Indian croplands and forests. We further found that the croplands SM-EVF relation exhibits a reversal in hysteresis in the case of root-zone SM. The surface SM-EVF hysteresis is not present in forests with large root depths and reduced soil evaporation due to high canopy shading, and yet it is present for the root-zone SM. With its reversal for croplands, the newly found hysteresis must be addressed in redefining the critical SM threshold to demarcate the energy and water-limiting regimes. It should be incorporated in the land surface modeling parameterization. Additionally, we observed hysteresis in the SM-gross primary productivity relationship across both land covers and soil profiles (surface and root-zone), underscoring the need to investigate such processes to consider their dynamics in future ecological and hydrological models.