Since almost couple of decades I am trying to develop tools that evaluate the surface water budget components, and I look at the closure of the budget equation. The outcomes of this research are our models GEOtop and our system JGrass-NewAGE, and some applications are listed below. My impression was that many researchers are talking of the water budget closure, since many actually have the knowledge and the tools for estimating the budget, but less are really doing it. We wrote (more or less) it in the introduction of one of our paper and we were asked by the reviewers to be more precise. The list below, certainly to be cleaned, improved and enriched, says that there are effectively many papers (out of around a hundred we inspected) that do it. They are distributed according to four threads.
- The one of “global and continental hydrology” where the water budget of the whole earth or of the largest river basins is studied. The methods used are remote sensing data, global circulation models, large-scale hydrological models.
- One is (but the focus is more often on evaporation) based on the use of Budyko curves, at various scales.
- The use models plus in-situ data, with various levels of simplification, usually from few kilometers to thousands of kilometers scales. Models are process-based (like CATHY, GEOtop or ParFlow, to cite three of them) or more conceptualised (as our JGrass-NewAGE). Data are the most various, depending on the spatial scale of the application and the type of model. Process-based models use more data (which is a richness or a weakness, depending on the point of view), while conceptual models use less data. Larger scale applications require a coarse graining of the data set and, obviously, a limitation in the description of spatial heterogeneity.
- Finally there are fully experimental papers, especially in forest and agricultural areas, with accurate measurements, for some specific plant stand, or even single trees.
In the selection of the paper below, I searched for the water budget equation, with all of the terms, its minimal expression being:
$\frac{\Delta S}{\Delta t} = P - ET - R$
where $S$ is the soil/groundwater storage, $P$ precipitation rate, $ET$ evapotranspiration, $R$ runoff. Various papers present a more articulated baudget, but certainly I did not listed the paper that not deals with the equation. Many papers, having “water budget” in the title, actually deal with evapotranspiration and were excluded. As Praveen Kumar (GS) argued to me, all good models preserve mass: but they often deal only with a part of the budget, and/or their authors are concerned with other specific topic. Also these papers (and some really very interesting were excluded). Finally, please find below the list. A different version of the same list (and its LaTeX editable version) with some comments about the spatial and temporal scales of the budget and some further information can be found here ( where references can be sorted).
P.S. - Another list (to review, just received from Roger Moussa) of water budget studies is here.
P.S. - Another list (to review, just received from Roger Moussa) of water budget studies is here.
References
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