of the energy required to change the temperature of a substance by a given
amount, differs greatly between common natural surfaces. For example, the thermal inertia of liq-
uid water is about twice as high as that of ice or snow; which in turn may be more than twice as
high as that of sand and soil, depending on the water content. With the same energy input from the
sun, significant small-scale temperature
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
political decision makers, water managers, stakeholders, practitioners
and the general public that the water management process needs to be reformed the process
will most likely fail. Here the main uncertainty is related to the question of to which extent
it will be possible to convince the various actors of the substance of the matter and motivate
them, so that a common understanding of the need
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf