The relative merits of open- And closed-path analysers for measurement of eddy fluxes

Global Change Biology

Volumn 2, Issue 3, 1996, Pages 241-253

  Leuning, Ray ^a   Judd, Murray J ^b  

^a CSIRO   (Australia)

^b THE NEW ZEALAND INSTITUTE FOR PLANT AND FOOD RESEARCH LIMITED   (New Zealand)

Author keywords

Eddy covariance; Trace gas fluxes

Indexed keywords

ANALYZER; CARBON DIOXIDE FLUX; EDDY COVARIANCE; INSTRUMENTATION; TRACE GAS FLUX; WATER VAPOUR FLUX;

EID: 0030497367     PISSN: 13541013     EISSN: None     Source Type: Journal    
DOI: 10.1111/j.1365-2486.1996.tb00076.x     Document Type: Article

References (7)

1. 2. Boundary-Layer Meteorology, 59, 243-256.
2. Judd MJ, Prendergrast PT, McAneney KJ (1993) Carbon dioxide and latent heat flux measurements in a windbreak-sheltered orchard. Agricultural and Forest Meteorology, 66, 193-210.
3. Kaimal JC, Wyngaard JC, Izumi Y, Cote OR (1972) Spectral characteristics of surface layer turbulence. Quarterly Journal of the Royal Meteorological Society, 98, 563-589.
4. Kaimal JC, Gaynor JE, Zimmerman HA, Zimmerman GA (1990) Minimizing flow distortion errors in a sonic anemometer. Boundary- Layer Meteorology, 53, 103-115.
5. Moore CJ (1986) Frequency response corrections for eddy correlation systems. Boundary-Layer Meteorology, 37, 17-35.
6. Ohtaki E (1985) On the similarity in atmospheric flucuations of carbon dioxide, water vapour and temperature over vegetated fields. Boundary-Layer Meteorology, 32, 25-37.
7. Ohtaki E, Matsui M (1982) Infra-red device for simultaneous measurement of atmospheric carbon dioxide and water vapour. Boundary-Layer Meteorolog 24, 109-119.