This paper outlines the first part of a series of research studies to inves
tigate the potential and approaches for using optical remote sensing to ass
ess vegetation water content. It first analyzes why most methods used as ap
proximations of vegetation water content (such as vegetation stress indices
, estimation of degree of curing and chlorophyll content) are not suitable
for retrieving water content at leaf level. It then documents the physical
basis supporting the use of remote sensing to directly detect vegetation wa
ter content in terms of Equivalent Water Thickness (EWT) at leaf level. Usi
ng laboratory measurements, the radiative transfer model PROSPECT and a sen
sitivity analysis, it shows that shortwave infrared (SWIR) is sensitive to
EWT but cannot be used alone to retrieve EWT because two other leaf paramet
ers (internal structure and dry matter) also influence leaf reflectance in
the SWIR, A combination of SWIR and NIR (only influenced by these two param
eters) is necessary to retrieve EWT at leaf level. These results set the ba
sis towards establishing operational techniques for the retrieval of EWT at
top-of-canopy and top-of-atmospheric levels. (C) 2001 Elsevier Science Inc
. All rights reserved.