{"title":"Seasonal patterns and hydrological regulations of root zone storage capacity across United States","authors":"Shuping Du, Shanhu Jiang, Liliang Ren, Yongwei Zhu, Hao Cui, Miao He, Chong-Yu Xu","doi":"10.1016/j.agrformet.2025.110428","DOIUrl":null,"url":null,"abstract":"Root zone storage capacity (S<sub>r</sub>) represents the maximum subsurface storage accessible to plant roots. It is primarily influenced by water availability and water demand, thus exhibiting temporal change in response to climate variations. Previous studies have primarily focused on the spatial patterns of S<sub>r</sub> across local to global scales; however, there remains a limited understanding of its temporal patterns, particularly in relation to seasonal changes. This work explores the seasonal behavior of S<sub>r</sub> for wet and dry seasons and the hydrological regulation of seasonal S<sub>r</sub>. We propose a seasonal modeling framework based on apportionment entropy, which considers the phase difference between water and energy. Within this framework, the PDM-FLEX hydrological model, an integration of the probability distributed model (PDM) with the FLEX lumped model, was employed to calculate catchment-scale S<sub>r</sub> for each season across 671 catchments in the contiguous United States. Results show that: i) this framework can effectively capture seasonal S<sub>r</sub>, with wet season S<sub>r</sub> (an average of 564 mm) generally being smaller than dry season S<sub>r</sub> (an average of 820 mm) for most catchments. In the west, plants routinely access deep water, leading to comparable S<sub>r</sub> for both wet and dry seasons. Incorporating seasonal S<sub>r</sub> into the hydrological model can improve simulation performance across time scales; ii) dry season S<sub>r</sub> is more responsive to hydroclimatic control compared to wet season S<sub>r</sub>, as plants in arid climates are more sensitive to water accessibility; and iii) during the wet season, low S<sub>r</sub> relative to precipitation leads to an unresponsive hydrological reaction. However, during the dry season, a routine correlation between S<sub>r</sub> and precipitation produces responsive hydrological behavior. These findings indicate that plants seasonally adapt their root systems and that these seasonal variations in S<sub>r</sub> would have significant hydrological implications.","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"53 1","pages":""},"PeriodicalIF":5.6000,"publicationDate":"2025-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Agricultural and Forest Meteorology","FirstCategoryId":"97","ListUrlMain":"https://doi.org/10.1016/j.agrformet.2025.110428","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"AGRONOMY","Score":null,"Total":0}
引用次数: 0
Abstract
Root zone storage capacity (Sr) represents the maximum subsurface storage accessible to plant roots. It is primarily influenced by water availability and water demand, thus exhibiting temporal change in response to climate variations. Previous studies have primarily focused on the spatial patterns of Sr across local to global scales; however, there remains a limited understanding of its temporal patterns, particularly in relation to seasonal changes. This work explores the seasonal behavior of Sr for wet and dry seasons and the hydrological regulation of seasonal Sr. We propose a seasonal modeling framework based on apportionment entropy, which considers the phase difference between water and energy. Within this framework, the PDM-FLEX hydrological model, an integration of the probability distributed model (PDM) with the FLEX lumped model, was employed to calculate catchment-scale Sr for each season across 671 catchments in the contiguous United States. Results show that: i) this framework can effectively capture seasonal Sr, with wet season Sr (an average of 564 mm) generally being smaller than dry season Sr (an average of 820 mm) for most catchments. In the west, plants routinely access deep water, leading to comparable Sr for both wet and dry seasons. Incorporating seasonal Sr into the hydrological model can improve simulation performance across time scales; ii) dry season Sr is more responsive to hydroclimatic control compared to wet season Sr, as plants in arid climates are more sensitive to water accessibility; and iii) during the wet season, low Sr relative to precipitation leads to an unresponsive hydrological reaction. However, during the dry season, a routine correlation between Sr and precipitation produces responsive hydrological behavior. These findings indicate that plants seasonally adapt their root systems and that these seasonal variations in Sr would have significant hydrological implications.
期刊介绍:
Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published.
Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.