نتایج جستجو برای: eddy covariance

تعداد نتایج: 44832  

Journal: :Tree physiology 2007
Joshua B Fisher Dennis D Baldocchi Laurent Misson Todd E Dawson Allen H Goldstein

At the leaf scale, it is a long-held assumption that stomata close at night in the absence of light, causing transpiration to decrease to zero. Energy balance models and evapotranspiration equations often rely on net radiation as an upper bound, and some models reduce evapotranspiration to zero at night when there is no solar radiation. Emerging research is showing, however, that transpiration ...

2008
Lucy R. Hutyra J. William Munger Elizabeth Hammond-Pyle Scott R. Saleska Natalia Restrepo-Coupe Bruce C. Daube Plinio B. de Camargo Steven C. Wofsy

The controls on uptake and release of CO2 by tropical rainforests, and the responses to a changing climate, are major uncertainties in global climate change models. Eddy-covariance measurements potentially provide detailed data on CO2 exchange and responses to the environment in these forests, but accurate estimates of the net ecosystem exchange of CO2 (NEE) and ecosystem respiration (Reco) req...

2000
Caroline J. Nichol Karl F. Huemmrich T. Andrew Black Paul G. Jarvis Charles L. Walthall John Grace Forrest G. Hall

Using a helicopter-mounted portable spectroradiometer and continuous eddy covariance data we were able to evaluate the photochemical reflectance index (PRI) as an indicator of canopy photosynthetic light-use efficiency (LUE) in four boreal forest species during the Boreal Ecosystem Atmosphere experiment (BOREAS). PRI was calculated from narrow waveband reflectance data and correlated with LUE c...

2014
S. B. Grimmond C. Stockdale

11 Airborne measurements within the urban mixing layer (360 m) over Greater London are used to quantify CO2 12 emissions at the meso-scale. Daytime CO2 fluxes, calculated by the Integrative Mass Boundary Layer (IMBL) 13 method, ranged from 46 to 104 μmol CO2 m -2 s -1 for four days in October 2011. The day-to-day variability of 14 IMBL fluxes is at the same order of magnitude as for surface edd...

2017
Fabien Gibert Grady J. Koch Jeffrey Y. Beyon Timothy W. Hilton Kenneth J. Davis Arlyn Andrews Pierre H. Flamant Upendra N. Singh FABIEN GIBERT GRADY J. KOCH JEFFREY Y. BEYON TIMOTHY W. HILTON KENNETH J. DAVIS UPENDRA N. SINGH

The vertical profiling of CO2 turbulent fluxes in the atmospheric boundary layer (ABL) is investigated using a coherent differential absorption lidar (CDIAL) operated nearby a tall tower in Wisconsin during June 2007. A CDIAL can perform simultaneous range-resolved CO2 DIAL and velocity measurements. The lidar eddy covariance technique is presented. The aims of the study are (i) an assessment o...

Journal: :Science 2003
Scott R Saleska Scott D Miller Daniel M Matross Michael L Goulden Steven C Wofsy Humberto R da Rocha Plinio B de Camargo Patrick Crill Bruce C Daube Helber C de Freitas Lucy Hutyra Michael Keller Volker Kirchhoff Mary Menton J William Munger Elizabeth Hammond Pyle Amy H Rice Hudson Silva

The net ecosystem exchange of carbon dioxide was measured by eddy covariance methods for 3 years in two old-growth forest sites near Santarém, Brazil. Carbon was lost in the wet season and gained in the dry season, which was opposite to the seasonal cycles of both tree growth and model predictions. The 3-year average carbon loss was 1.3 (confidence interval: 0.0 to 2.0) megagrams of carbon per ...

2001
Werner Eugster Reto Burkard Otto Klemm Thomas Wrzesinsky

The eddy covariance method is considered the only direct flux measurement method. Its application for fog deposition measurements is relatively new and has a high potential to allow the accurate determination of nutrient and trace element deposition due to fog droplet interception by vegetation canopies. Based on experiences gained at an agricultural site on the Swiss Plateau and a mountainous ...

Journal: :Science 2001
C C Barford S C Wofsy M L Goulden J W Munger E H Pyle S P Urbanski L Hutyra S R Saleska D Fitzjarrald K Moore

Net uptake of carbon dioxide (CO2) measured by eddy covariance in a 60- to 80-year-old forest averaged 2.0 +/- 0.4 megagrams of carbon per hectare per year during 1993 to 2000, with interannual variations exceeding 50%. Biometry indicated storage of 1.6 +/- 0.4 megagrams of carbon per hectare per year over 8 years, 60% in live biomass and the balance in coarse woody debris and soils, confirming...

Journal: :Journal of Geophysical Research: Biogeosciences 2017

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