{"title":"高寒生态系统能量平衡和蒸腾分数的年代际动态:模拟和观测研究","authors":"Yao Wu, Pei Wang","doi":"10.1002/eco.70029","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>Evapotranspiration (<i>ET</i>) is a critical component of the soil–plant–atmosphere continuum, significantly influencing the water and energy balance of ecosystems. However, existing studies on <i>ET</i> have primarily focused on the growing season or specific years, with limited long-term analyses spanning decades. This study aims to analyse the components of <i>ET</i> within the alpine ecosystem of the Heihe River Basin, specifically investigating the dynamics of vegetation transpiration (<i>T</i>) and soil evaporation (<i>Ev</i>). Utilizing the <i>SPAC</i> model and integrating meteorological observations and eddy covariance data from 2013 to 2022, we investigate the impact of solar radiation and vegetation dynamics on <i>ET</i> and its partitioning (<i>T</i>/<i>ET</i>). The agreement between measured and simulated energy fluxes (net radiation and latent energy flux) and soil temperature underscores the validity of the model's performance. Additionally, a comparison employing the underlying water use efficiency method reveals consistent <i>T</i>/<i>ET</i> values during the growing season, further confirming the model's accuracy. Results indicate that the annual average <i>T</i>/<i>ET</i> during the 10-year study period is 0.41 ± 0.03, close to the global average but lower than in warmer, humid regions. Seasonal analysis reveals a significant increase in <i>T</i>/<i>ET</i> during the growing season (April to October), particularly in May and June, coinciding with the thawing of permafrost and increased soil moisture. In addition, the study finds that the leaf area index and canopy stomatal conductance exhibit a logarithmic relationship with <i>T</i>/<i>ET</i>, whereas soil temperature and downward longwave radiation show an exponential relationship with <i>T</i>/<i>ET</i>. This study highlights the importance of understanding the stomatal conductance dynamics and their controls of transpiration process within alpine ecosystems. By providing key insights into the hydrological processes of these environments, it offers guidance for adapting to climate change impacts.</p>\n </div>","PeriodicalId":55169,"journal":{"name":"Ecohydrology","volume":"18 2","pages":""},"PeriodicalIF":2.5000,"publicationDate":"2025-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Decadal Dynamics of Energy Balance and Transpiration Fraction in an Alpine Ecosystem: A Modelling and Observational Study\",\"authors\":\"Yao Wu, Pei Wang\",\"doi\":\"10.1002/eco.70029\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n <p>Evapotranspiration (<i>ET</i>) is a critical component of the soil–plant–atmosphere continuum, significantly influencing the water and energy balance of ecosystems. However, existing studies on <i>ET</i> have primarily focused on the growing season or specific years, with limited long-term analyses spanning decades. This study aims to analyse the components of <i>ET</i> within the alpine ecosystem of the Heihe River Basin, specifically investigating the dynamics of vegetation transpiration (<i>T</i>) and soil evaporation (<i>Ev</i>). Utilizing the <i>SPAC</i> model and integrating meteorological observations and eddy covariance data from 2013 to 2022, we investigate the impact of solar radiation and vegetation dynamics on <i>ET</i> and its partitioning (<i>T</i>/<i>ET</i>). The agreement between measured and simulated energy fluxes (net radiation and latent energy flux) and soil temperature underscores the validity of the model's performance. Additionally, a comparison employing the underlying water use efficiency method reveals consistent <i>T</i>/<i>ET</i> values during the growing season, further confirming the model's accuracy. Results indicate that the annual average <i>T</i>/<i>ET</i> during the 10-year study period is 0.41 ± 0.03, close to the global average but lower than in warmer, humid regions. Seasonal analysis reveals a significant increase in <i>T</i>/<i>ET</i> during the growing season (April to October), particularly in May and June, coinciding with the thawing of permafrost and increased soil moisture. In addition, the study finds that the leaf area index and canopy stomatal conductance exhibit a logarithmic relationship with <i>T</i>/<i>ET</i>, whereas soil temperature and downward longwave radiation show an exponential relationship with <i>T</i>/<i>ET</i>. This study highlights the importance of understanding the stomatal conductance dynamics and their controls of transpiration process within alpine ecosystems. By providing key insights into the hydrological processes of these environments, it offers guidance for adapting to climate change impacts.</p>\\n </div>\",\"PeriodicalId\":55169,\"journal\":{\"name\":\"Ecohydrology\",\"volume\":\"18 2\",\"pages\":\"\"},\"PeriodicalIF\":2.5000,\"publicationDate\":\"2025-03-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Ecohydrology\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/eco.70029\",\"RegionNum\":3,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ECOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ecohydrology","FirstCategoryId":"93","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/eco.70029","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ECOLOGY","Score":null,"Total":0}
Decadal Dynamics of Energy Balance and Transpiration Fraction in an Alpine Ecosystem: A Modelling and Observational Study
Evapotranspiration (ET) is a critical component of the soil–plant–atmosphere continuum, significantly influencing the water and energy balance of ecosystems. However, existing studies on ET have primarily focused on the growing season or specific years, with limited long-term analyses spanning decades. This study aims to analyse the components of ET within the alpine ecosystem of the Heihe River Basin, specifically investigating the dynamics of vegetation transpiration (T) and soil evaporation (Ev). Utilizing the SPAC model and integrating meteorological observations and eddy covariance data from 2013 to 2022, we investigate the impact of solar radiation and vegetation dynamics on ET and its partitioning (T/ET). The agreement between measured and simulated energy fluxes (net radiation and latent energy flux) and soil temperature underscores the validity of the model's performance. Additionally, a comparison employing the underlying water use efficiency method reveals consistent T/ET values during the growing season, further confirming the model's accuracy. Results indicate that the annual average T/ET during the 10-year study period is 0.41 ± 0.03, close to the global average but lower than in warmer, humid regions. Seasonal analysis reveals a significant increase in T/ET during the growing season (April to October), particularly in May and June, coinciding with the thawing of permafrost and increased soil moisture. In addition, the study finds that the leaf area index and canopy stomatal conductance exhibit a logarithmic relationship with T/ET, whereas soil temperature and downward longwave radiation show an exponential relationship with T/ET. This study highlights the importance of understanding the stomatal conductance dynamics and their controls of transpiration process within alpine ecosystems. By providing key insights into the hydrological processes of these environments, it offers guidance for adapting to climate change impacts.
期刊介绍:
Ecohydrology is an international journal publishing original scientific and review papers that aim to improve understanding of processes at the interface between ecology and hydrology and associated applications related to environmental management.
Ecohydrology seeks to increase interdisciplinary insights by placing particular emphasis on interactions and associated feedbacks in both space and time between ecological systems and the hydrological cycle. Research contributions are solicited from disciplines focusing on the physical, ecological, biological, biogeochemical, geomorphological, drainage basin, mathematical and methodological aspects of ecohydrology. Research in both terrestrial and aquatic systems is of interest provided it explicitly links ecological systems and the hydrologic cycle; research such as aquatic ecological, channel engineering, or ecological or hydrological modelling is less appropriate for the journal unless it specifically addresses the criteria above. Manuscripts describing individual case studies are of interest in cases where broader insights are discussed beyond site- and species-specific results.