(1996), we would not describe the studied processes by means of differential equations that
characterize mass flow, impulse, or different
forms of energy.
SAM makes it possible to reveal and describe
quantitatively a set of basic processes and their
relations to environmental factors (i.e. structural–
functional organization) for little-studied natural
systems. For instance, SAM enabled to detect of
short temperature-independent 1–3-day periods
in plant annual development as well as to estimate quantitatively a vertical diffusion and condensation of vaporous water in soils throughout a
year (Kirsta 2006a, b). SAM provides the
Fig. 7.1 Climate destabilization areas were established via spatial clustering of precipitation in Eurasia (see weather
stations marked by a large circle) (Kirsta et al. 2014)
Fig. 7.2 Climate destabilization areas were established via spatial clustering of air temperature in Eurasia (see weather
stations marked by a large circle) (Kirsta et al. 2014)
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Y. Kirsta and A. Puzanov
characterize mass flow, impulse, or different
forms of energy.
SAM makes it possible to reveal and describe
quantitatively a set of basic processes and their
relations to environmental factors (i.e. structural–
functional organization) for little-studied natural
systems. For instance, SAM enabled to detect of
short temperature-independent 1–3-day periods
in plant annual development as well as to estimate quantitatively a vertical diffusion and condensation of vaporous water in soils throughout a
year (Kirsta 2006a, b). SAM provides the
Fig. 7.1 Climate destabilization areas were established via spatial clustering of precipitation in Eurasia (see weather
stations marked by a large circle) (Kirsta et al. 2014)
Fig. 7.2 Climate destabilization areas were established via spatial clustering of air temperature in Eurasia (see weather
stations marked by a large circle) (Kirsta et al. 2014)
82
Y. Kirsta and A. Puzanov