At present a network of over 100 field sites are measuring carbon dioxide,
water vapor and sensible heat fluxes between the biosphere and atmosphere,
on a nearly continuous basis. Gaps in the long term measurements of evapora
tion and sensible heat flux must be filled before these data can be used fo
r hydrological and meteorological applications. We adapted methods of gap f
illing for NEE (net ecosystem exchange of carbon) to energy fluxes and appl
ied them to data sets available from the EUROFLUX and AmeriFlux eddy covari
ance databases. The average data coverage for the sites selected was 69% an
d 75% for latent heat (lambdaE) and sensible heat (H). The methods were bas
ed on mean diurnal variations (half-hourly binned means of fluxes based on
previous and subsequent days, MDV) and look-up tables for fluxes during ass
orted meteorological conditions (LookUp), and the impact of different gap f
illing methods on the annual sum of lambdaE and H is investigated. The diff
erence between annual lambdaE filled by MDV and lambdaE filled by LookUp ra
nged from -120 to 210 MJ m(-2) per year, i.e. -48 to +86 mm per year, or -1
3 to +39% of the annual sum. For annual sums of H differences between - 140
and +140 MJ m(-2) per year or -12 to +19% of the annual sum were found. (C
) 2001 Elsevier Science B.V. All rights reserved.