The role of the land surface in controlling climate is still underestimated
and access to information from the boreal-forest zone is instrumental to i
mprove this situation. This motivated the organisation of NOPEX (Northern h
emisphere climate-Processes land-surface Experiment) in the southern part o
f the European boreal zone. This paper summarises results from NOPEX in its
first phase, dealing with spring- and summertime conditions. Two concentra
ted field efforts (CFE1 on 27 May-23 June 1994, CFE2 on 18 April-14 July 19
95) were carried out with coordinated measurements of energy, water, and CO
2 budgets at 13 ground-based sites and at various airborne platforms. Flux
aggregation was a central issue in the heterogeneous, patchy NOPEX landscap
e. It is shown that simple land-use-weighted averaging of fluxes from field
s/forests/lakes agree well with regional fluxes. Momentum fluxes can be par
ameterised over the whole area with a roughness length of approximately 1.5
m, whereas fluxes of sensible heat and other scalars depend on the averagi
ng scale, Local measurements of soil moisture can be classified and meaning
ful averages can be deduced with a 1 km resolution. Lakes play an important
role and differs in both diurnal and annual cycles compared to the forests
and fields. Multiannual data from an agricultural and a forest site has al
lowed quantification and modelling of seldom occuring phenomena. One unexpe
cted result was that the Norunda Common forest acted as a source and not a
sink of CO2. The successful completion of CFE1-2 and a pilot winter campaig
n (CFE3) will lead NOPEX into its final phase, devoted to wintertime proces
ses. Measurements and model results reside in SINOP. the System for Informa
tion in NOPEX, open for NOPEX participants. Data from CFE1 and CFE2 are rel
eased on CD as an integrated part of this Special Issue. (C) 1999 Elsevier
Science B.V. All rights reserved.