DIURNAL HYSTERESES OF STOMATAL AND BULK SURFACE CONDUCTANCES IN RELATION TO VAPOR-PRESSURE DEFICIT IN A COOL-TEMPERATE WETLAND
Citation
K. Takagi et al., DIURNAL HYSTERESES OF STOMATAL AND BULK SURFACE CONDUCTANCES IN RELATION TO VAPOR-PRESSURE DEFICIT IN A COOL-TEMPERATE WETLAND, Agricultural and forest meteorology, 91(3-4), 1998, pp. 177-191
Categorie Soggetti
Agriculture,Forestry,"Metereology & Atmospheric Sciences
SICI code
0168-1923(1998)91:3-4<177:DHOSAB>2.0.ZU;2-7
Abstract
In order to evaluate the stomatal control on the canopy evapotranspira
tion, diurnal variations in stomatal conductance (g(s)) of individual
plants and bulk surface conductance (G(s)) of the canopy were measured
independently in the Sarobetsu mire of northern Japan. During July-Au
gust 1993 and 1994, g(s) was measured for four species (Sasa palmata,
Moliniopsis japonica, Myrica gale L. var. tomentosa and Ilex crenata v
ar. paludosa) growing in the mire. In July and August 1995, G(s) was d
etermined using Penman-Monteith equation. In this equation, evapotrans
piration rate was determined by the Bowen ratio/energy balance method.
Diurnal hysteresis curves of g(s) in relation to leaf-to-air vapor pr
essure deficit (nu) followed different courses from day to day accordi
ng to the magnitude of nu, and daily maximum g(s) was correlated negat
ively with daily maximum nu except for Ilex crenata var. paludosa. Sim
ilar clockwise hysteresis curves were observed between G(s) and Vapor
pressure deficit at the mean evaporative surface (D-0), and daily maxi
mum G(s) decreased with daily maximum D-0 in midsummer. In particular,
on days when daily maximum D-0 increased up to 1.9 kPa, the large dec
rease in G(s) decreased the evapotranspiration rate, despite high irra
diance levels. Thus, stomatal control by individual plant leaves stron
gly affects evapotranspiration from the canopy and prevents excessive
water loss on days when vapor pressure deficit is high, even when soil
water is plentiful. On the rising limb of the diurnal course of the t
ranspiration rate (T-r), increases in T-r with change in nu, Delta T-r
/Delta nu varied from day to day, in particular for M. gale L. var, to
mentosa. Further, a negative relationship was found between Delta T-r/
Delta nu and the rate of increase of nu for unit change in time. We be
lieve that the change of the daily course of g(s) and T-r was caused b
y the response of stomata to the increased rate of change of nu. Thus,
in order to predict the diurnal variation of g(s), the magnitude and
tendency of nu for each day must be considered. (C) 1998 Elsevier Scie
nce B.V. All rights reserved.