Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau
Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been wi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Binbin [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. |
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| Übergeordnetes Werk: |
Enthalten in: Journal of geophysical research / D - Washington, DC : Union, 1984, 122(2017), 4, Seite 2289-2303 |
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| Übergeordnetes Werk: |
volume:122 ; year:2017 ; number:4 ; pages:2289-2303 |
| Links: |
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| DOI / URN: |
10.1002/2016JD026109 |
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OLC1992962731 |
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| 245 | 1 | 0 | |a Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau |
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| 520 | |a Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season | ||
| 540 | |a Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. | ||
| 650 | 4 | |a high altitude | |
| 650 | 4 | |a small lakes | |
| 650 | 4 | |a evaporation | |
| 650 | 4 | |a energy budget | |
| 650 | 4 | |a Nam Co | |
| 650 | 4 | |a Tibetan Plateau | |
| 650 | 4 | |a Meteorology | |
| 650 | 4 | |a Lakes | |
| 650 | 4 | |a Geophysics | |
| 650 | 4 | |a Turbulence | |
| 650 | 4 | |a Evaporation | |
| 700 | 1 | |a Ma, Yaoming |4 oth | |
| 700 | 1 | |a Ma, Weiqiang |4 oth | |
| 700 | 1 | |a Su, Zhongbo |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t Journal of geophysical research / D |d Washington, DC : Union, 1984 |g 122(2017), 4, Seite 2289-2303 |w (DE-627)130444391 |w (DE-600)710256-2 |w (DE-576)015978818 |x 2169-897X |7 nnns |
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10.1002/2016JD026109 doi PQ20170721 (DE-627)OLC1992962731 (DE-599)GBVOLC1992962731 (PRQ)p2197-e9e93b97a88690d7118b6287b79ff31063ae9e8739d34b006cd0899d0c7a21270 (KEY)0137985220170000122000402289physicalcontrolsonhalfhourlydailyandmonthlyturbule DE-627 ger DE-627 rakwb eng 550 DNB Wang, Binbin verfasserin aut Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. high altitude small lakes evaporation energy budget Nam Co Tibetan Plateau Meteorology Lakes Geophysics Turbulence Evaporation Ma, Yaoming oth Ma, Weiqiang oth Su, Zhongbo oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 4, Seite 2289-2303 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:4 pages:2289-2303 http://dx.doi.org/10.1002/2016JD026109 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2016JD026109/abstract https://search.proquest.com/docview/1876699578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 4 2289-2303 |
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10.1002/2016JD026109 doi PQ20170721 (DE-627)OLC1992962731 (DE-599)GBVOLC1992962731 (PRQ)p2197-e9e93b97a88690d7118b6287b79ff31063ae9e8739d34b006cd0899d0c7a21270 (KEY)0137985220170000122000402289physicalcontrolsonhalfhourlydailyandmonthlyturbule DE-627 ger DE-627 rakwb eng 550 DNB Wang, Binbin verfasserin aut Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. high altitude small lakes evaporation energy budget Nam Co Tibetan Plateau Meteorology Lakes Geophysics Turbulence Evaporation Ma, Yaoming oth Ma, Weiqiang oth Su, Zhongbo oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 4, Seite 2289-2303 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:4 pages:2289-2303 http://dx.doi.org/10.1002/2016JD026109 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2016JD026109/abstract https://search.proquest.com/docview/1876699578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 4 2289-2303 |
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10.1002/2016JD026109 doi PQ20170721 (DE-627)OLC1992962731 (DE-599)GBVOLC1992962731 (PRQ)p2197-e9e93b97a88690d7118b6287b79ff31063ae9e8739d34b006cd0899d0c7a21270 (KEY)0137985220170000122000402289physicalcontrolsonhalfhourlydailyandmonthlyturbule DE-627 ger DE-627 rakwb eng 550 DNB Wang, Binbin verfasserin aut Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. high altitude small lakes evaporation energy budget Nam Co Tibetan Plateau Meteorology Lakes Geophysics Turbulence Evaporation Ma, Yaoming oth Ma, Weiqiang oth Su, Zhongbo oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 4, Seite 2289-2303 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:4 pages:2289-2303 http://dx.doi.org/10.1002/2016JD026109 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2016JD026109/abstract https://search.proquest.com/docview/1876699578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 4 2289-2303 |
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10.1002/2016JD026109 doi PQ20170721 (DE-627)OLC1992962731 (DE-599)GBVOLC1992962731 (PRQ)p2197-e9e93b97a88690d7118b6287b79ff31063ae9e8739d34b006cd0899d0c7a21270 (KEY)0137985220170000122000402289physicalcontrolsonhalfhourlydailyandmonthlyturbule DE-627 ger DE-627 rakwb eng 550 DNB Wang, Binbin verfasserin aut Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. high altitude small lakes evaporation energy budget Nam Co Tibetan Plateau Meteorology Lakes Geophysics Turbulence Evaporation Ma, Yaoming oth Ma, Weiqiang oth Su, Zhongbo oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 4, Seite 2289-2303 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:4 pages:2289-2303 http://dx.doi.org/10.1002/2016JD026109 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2016JD026109/abstract https://search.proquest.com/docview/1876699578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 4 2289-2303 |
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10.1002/2016JD026109 doi PQ20170721 (DE-627)OLC1992962731 (DE-599)GBVOLC1992962731 (PRQ)p2197-e9e93b97a88690d7118b6287b79ff31063ae9e8739d34b006cd0899d0c7a21270 (KEY)0137985220170000122000402289physicalcontrolsonhalfhourlydailyandmonthlyturbule DE-627 ger DE-627 rakwb eng 550 DNB Wang, Binbin verfasserin aut Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season Nutzungsrecht: © 2017. American Geophysical Union. All Rights Reserved. high altitude small lakes evaporation energy budget Nam Co Tibetan Plateau Meteorology Lakes Geophysics Turbulence Evaporation Ma, Yaoming oth Ma, Weiqiang oth Su, Zhongbo oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 122(2017), 4, Seite 2289-2303 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:122 year:2017 number:4 pages:2289-2303 http://dx.doi.org/10.1002/2016JD026109 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2016JD026109/abstract https://search.proquest.com/docview/1876699578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 122 2017 4 2289-2303 |
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Wang, Binbin |
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Wang, Binbin ddc 550 misc high altitude misc small lakes misc evaporation misc energy budget misc Nam Co misc Tibetan Plateau misc Meteorology misc Lakes misc Geophysics misc Turbulence misc Evaporation Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau |
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550 DNB Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau high altitude small lakes evaporation energy budget Nam Co Tibetan Plateau Meteorology Lakes Geophysics Turbulence Evaporation |
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Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau |
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physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the tibetan plateau |
| title_auth |
Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau |
| abstract |
Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season |
| abstractGer |
Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season |
| abstract_unstemmed |
Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment‐scale water balance analysis and local‐scale climate modeling. The observation and simulation of lake‐air turbulent flux processes have been widely carried out, but studies that examine high‐altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four‐component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long‐term evaporation and energy budget observations. With the valuable measurements collected during the ice‐free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812 mm) is approximately 200 mm larger than that from adjacent Nam Co (approximately 627 mm) during their ice‐free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake‐air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97. The evaporation from a small lake on the Tibetan Plateau, about 812 mm over the entire ice‐free season, is reported for the first time U z has weaker correlation over temporal scales of daily and monthly than half hourly, and Δ E has no contribution under neutral conditions The energy budget, with an estimated closure value of 0.97, is generally balanced over the entire ice‐free season |
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Physical controls on half‐hourly, daily, and monthly turbulent flux and energy budget over a high‐altitude small lake on the Tibetan Plateau |
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http://dx.doi.org/10.1002/2016JD026109 http://onlinelibrary.wiley.com/doi/10.1002/2016JD026109/abstract https://search.proquest.com/docview/1876699578 |
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Ma, Yaoming Ma, Weiqiang Su, Zhongbo |
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