Seasonal variations in the evapotranspiration of a transitional tropical forest of Mato Grosso, Brazil
The seasonal pattern of evapotranspiration (expressed as latent heat flux Qe) for a 28‐ to 30‐m‐tall tropical transitional (ecotonal) forest was quantified over an annual cycle using eddy covariance measurement and micrometeorological estimation techniques. The study was conducted near the city of S...
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| Published in: | Water resources research Vol. 38; no. 6; pp. 30-1 - 30-11 |
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| Main Authors: | , , , , , |
| Format: | Journal Article |
| Language: | English |
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American Geophysical Union
01-06-2002
Blackwell Publishing Ltd |
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| Abstract | The seasonal pattern of evapotranspiration (expressed as latent heat flux Qe) for a 28‐ to 30‐m‐tall tropical transitional (ecotonal) forest was quantified over an annual cycle using eddy covariance measurement and micrometeorological estimation techniques. The study was conducted near the city of Sinop, in northern Mato Grosso, Brazil, which is located within the ecotone of tropical rain forest and savanna (cerrado). Although the majority of net radiation (Q*) was consumed by Qe (50–90%), seasonal variations in Qe were large and positively correlated with precipitation. Total daily Qe for the dry season (June–September) was on average 6.0 MJ m−2 d−1, while daily Qe for the transition (October–November and April–May) and wet (December–March) season periods were 7.5 and 10.0 MJ m−2 d−1, respectively. The seasonal variation in midday (0900–1500 LT) surface conductance (gs) was also positively correlated with precipitation. Analysis of the “decoupling factor” (Ω) indicated that the forest was strongly coupled to the atmosphere (Ω = 0.1–0.3) over the dry season and transition periods, suggesting that Qe was under relatively strong stomatal control. Although rainfall during the study period was above the long‐term (30‐year) average, our results indicate that the seasonal dynamics of Qe for the tropical transitional forest were more comparable to tropical savanna than to rain forest. |
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| AbstractList | The seasonal pattern of evapotranspiration (expressed as latent heat flux Qe) for a 28‐ to 30‐m‐tall tropical transitional (ecotonal) forest was quantified over an annual cycle using eddy covariance measurement and micrometeorological estimation techniques. The study was conducted near the city of Sinop, in northern Mato Grosso, Brazil, which is located within the ecotone of tropical rain forest and savanna (cerrado). Although the majority of net radiation (Q*) was consumed by Qe (50–90%), seasonal variations in Qe were large and positively correlated with precipitation. Total daily Qe for the dry season (June–September) was on average 6.0 MJ m−2 d−1, while daily Qe for the transition (October–November and April–May) and wet (December–March) season periods were 7.5 and 10.0 MJ m−2 d−1, respectively. The seasonal variation in midday (0900–1500 LT) surface conductance (gs) was also positively correlated with precipitation. Analysis of the “decoupling factor” (Ω) indicated that the forest was strongly coupled to the atmosphere (Ω = 0.1–0.3) over the dry season and transition periods, suggesting that Qe was under relatively strong stomatal control. Although rainfall during the study period was above the long‐term (30‐year) average, our results indicate that the seasonal dynamics of Qe for the tropical transitional forest were more comparable to tropical savanna than to rain forest. The seasonal pattern of evapotranspiration (expressed as latent heat flux Q sub(e)) for a 28-to 30-m-tall tropical transitional (ecotonal) forest was quantified over an annual cycle using eddy covariance measurement and micrometeorological estimation techniques. The study was conducted near the city of Sinop, in northern Mato Grosso, Brazil, which is located within the ecotone of tropical rain forest and savanna (cerrado). Although the majority of net radiation (Q*) was consumed by Q sub(e) (50-90%), seasonal variations in Q sub(e) were large and positively correlated with precipitation. Total daily Q sub(e) for the dry season (June-August) was on average 6.0 MJ m super(-2) d super(-1) , while daily Q sub(e) for the transition (October-November and April-May) and wet (December-March) season periods were 7.5 and 10.0 MJ m super(-2) d super(-1), respectively. The seasonal variation in midday (0900-1500 LT) surface conductance (g sub(s)) was also positively correlated with precipitation. Analysis of the "decoupling factor" ( Omega ) indicated that the forest was strongly coupled to the atmosphere ( Omega = 0.1-0.3) over the dry season and transition periods, suggesting that Q sub(e) was under relatively strong stomatal control. Athough rainfall during the study period was above the long-term (30-year) average, our results indicate that seasonal dynamics of Q sub(e) for the tropical transitional forest were more comparable to tropical savanna than to rain forest. The seasonal pattern of evapotranspiration (expressed as latent heat flux Q e ) for a 28‐ to 30‐m‐tall tropical transitional (ecotonal) forest was quantified over an annual cycle using eddy covariance measurement and micrometeorological estimation techniques. The study was conducted near the city of Sinop, in northern Mato Grosso, Brazil, which is located within the ecotone of tropical rain forest and savanna (cerrado). Although the majority of net radiation ( Q *) was consumed by Q e (50–90%), seasonal variations in Q e were large and positively correlated with precipitation. Total daily Q e for the dry season (June–September) was on average 6.0 MJ m −2 d −1 , while daily Q e for the transition (October–November and April–May) and wet (December–March) season periods were 7.5 and 10.0 MJ m −2 d −1 , respectively. The seasonal variation in midday (0900–1500 LT) surface conductance ( g s ) was also positively correlated with precipitation. Analysis of the “decoupling factor” (Ω) indicated that the forest was strongly coupled to the atmosphere (Ω = 0.1–0.3) over the dry season and transition periods, suggesting that Q e was under relatively strong stomatal control. Although rainfall during the study period was above the long‐term (30‐year) average, our results indicate that the seasonal dynamics of Q e for the tropical transitional forest were more comparable to tropical savanna than to rain forest. |
| Author | Mauro M. S. Hayashi George L. Vourlitis José Holanda Campelo Jr Nicolau Priante Filho Fernando T. Caseiro José de S. Nogueira |
| Author_xml | – sequence: 1 givenname: George L. surname: Vourlitis fullname: Vourlitis, George L. organization: Biological Sciences Department, California State University, California, San Marcos, USA – sequence: 2 givenname: Nicolau Priante surname: Filho fullname: Filho, Nicolau Priante organization: Departamento de Física, Universidade Federal de Mato Grosso, Mato Grosso, Cuiabá, Brazil – sequence: 3 givenname: Mauro M. S. surname: Hayashi fullname: Hayashi, Mauro M. S. organization: Núcleo de Tecnologia em Armazenagem, Universidade Federal de Mato Grosso, Mato Grosso, Cuiabá, Brazil – sequence: 4 givenname: José surname: de S. Nogueira fullname: de S. Nogueira, José organization: Departamento de Física, Universidade Federal de Mato Grosso, Mato Grosso, Cuiabá, Brazil – sequence: 5 givenname: Fernando T. surname: Caseiro fullname: Caseiro, Fernando T. organization: Núcleo de Tecnologia em Armazenagem, Universidade Federal de Mato Grosso, Mato Grosso, Cuiabá, Brazil – sequence: 6 givenname: José Holanda surname: Campelo Jr fullname: Campelo Jr, José Holanda organization: Núcleo de Tecnologia em Armazenagem, Universidade Federal de Mato Grosso, Mato Grosso, Cuiabá, Brazil |
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| Copyright | 2008 American Geophysical Union Copyright 2002 by the American Geophysical Union. |
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| Snippet | The seasonal pattern of evapotranspiration (expressed as latent heat flux Qe) for a 28‐ to 30‐m‐tall tropical transitional (ecotonal) forest was quantified... The seasonal pattern of evapotranspiration (expressed as latent heat flux Q e ) for a 28‐ to 30‐m‐tall tropical transitional (ecotonal) forest was quantified... The seasonal pattern of evapotranspiration (expressed as latent heat flux Q sub(e)) for a 28-to 30-m-tall tropical transitional (ecotonal) forest was... |
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| SubjectTerms | Brazil, Mato Grosso, Sinop Canopy conductance decoupling factor energy balance Evapotranspiration Hydrologic budget Hydrology Meteorology and Atmospheric Dynamics micrometeorology Plant ecology Priestley-Taylor alpha Tropical meteorology Water/energy interactions |
| Title | Seasonal variations in the evapotranspiration of a transitional tropical forest of Mato Grosso, Brazil |
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