2019
DOI: 10.1016/j.scitotenv.2018.09.130
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A comprehensive analysis of interseasonal and interannual energy and water balance dynamics in semiarid shrubland and forest ecosystems

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Cited by 15 publications
(8 citation statements)
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“…For long‐term water balance in large natural catchments, evapotranspiration can be regarded as the partitioning of precipitation which is serving as water availability in Budyko formulations (ET=PR) while water storage is assumed to be negligible (Donohue et al, 2010; Hobbins et al, 2001; Rodell, 2004; Xue et al, 2013). Recently, the estimation of water balance at finer time scales has attracted more attentions in many studies and these studies showed that the water storage change (including soil moisture and groundwater) played a significant role in annual water balance and made a great contribution to meet the deficit of water supply for crop water demand (Chen et al, 2018; Flerchinger & Cooley, 2000; Ghamarnia et al, 2013; Leblanc et al, 2009; Valayamkunnath et al, 2019). The application of equivalent precipitation incorporating water storage change is able to work better at improving the performance of Budyko predictions in annual scale (Chen et al, 2013; Istanbulluoglu et al, 2012; Naumburg et al, 2005; Wang, 2012; Wang & Zhou, 2016), especially for basins in arid and semi‐arid regions (Du et al, 2016; Milly & Dunne, 2002; Xing et al, 2018).…”
Section: Discussionmentioning
confidence: 99%
“…For long‐term water balance in large natural catchments, evapotranspiration can be regarded as the partitioning of precipitation which is serving as water availability in Budyko formulations (ET=PR) while water storage is assumed to be negligible (Donohue et al, 2010; Hobbins et al, 2001; Rodell, 2004; Xue et al, 2013). Recently, the estimation of water balance at finer time scales has attracted more attentions in many studies and these studies showed that the water storage change (including soil moisture and groundwater) played a significant role in annual water balance and made a great contribution to meet the deficit of water supply for crop water demand (Chen et al, 2018; Flerchinger & Cooley, 2000; Ghamarnia et al, 2013; Leblanc et al, 2009; Valayamkunnath et al, 2019). The application of equivalent precipitation incorporating water storage change is able to work better at improving the performance of Budyko predictions in annual scale (Chen et al, 2013; Istanbulluoglu et al, 2012; Naumburg et al, 2005; Wang, 2012; Wang & Zhou, 2016), especially for basins in arid and semi‐arid regions (Du et al, 2016; Milly & Dunne, 2002; Xing et al, 2018).…”
Section: Discussionmentioning
confidence: 99%
“…For long-term water balance in large natural catchments, evapotranspiration can be regarded as the partitioning of precipitation which is serving as water availability in Budyko formulations ( = − ) while water storage is assumed to be negligible (Donohue et al, 2010;Hobbins et al, 2001;Rodell, 2004;Xue et al, 2013). Recently, the estimation of water balance at finer time scales has attracted more attentions in many studies and these studies showed that the water storage change (including soil moisture and groundwater) played a significant role in annual water balance and made a great contribution to meet the deficit of water supply for crop water demand (Chen et al, 2018;Flerchinger and Cooley, 2000;Ghamarnia et al, 2013;Leblanc et al, 2009;Namuburg et al, 2005;Valayamkunnath et al, 2019). The application of equivalent precipitation incorporating water storage change is able to work better at improving the performance of Budyko predictions in annual scale Istanbulluoglu et al, 2012;Wang, 2012;Wang and Zhou, 2016), especially for basins in arid and semi-arid regions (Du et al, 2016;Milly and Dunne, 2002;Xing et al, 2018).…”
Section: Uncertainty About the Annual Water Balance And Influence Factors On ωmentioning
confidence: 99%
“…Changes in albedo, canopy conditions, soil and litter characteristics as well as different water use strategies by natural forests compared with tea plantations have profound effects on local water balance and energy budget (Lai et al, 2018; Zhou et al, 2020). Water balance of forest ecosystem was comprehensively influenced by the hydrological characteristics of different functional layers (e.g., canopy, litter and soil layers) (Aguilos et al, 2021; Souza‐Alonso et al, 2022; Valayamkunnath et al, 2019a). However, previous studies on water balance response to land‐use conversion of natural forests and managed tea plantations have mainly focused on soil layer (Lai et al, 2018; Liao et al, 2016; Zhu et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
“…balance of forest ecosystem was comprehensively influenced by the hydrological characteristics of different functional layers (e.g., canopy, litter and soil layers) (Aguilos et al, 2021;Souza-Alonso et al, 2022;Valayamkunnath et al, 2019a). However, previous studies on water balance response to land-use conversion of natural forests and managed tea plantations have mainly focused on soil layer (Lai et al, 2018;Liao et al, 2016;Zhu et al, 2014).…”
mentioning
confidence: 99%