Although several attempts have been made in both sides, limitations and problems of current approach still remain.
Changes in runoff resulting from heterogeneous wildfire effects are not well-understood due to both limitations in the field measurement of runoff and temporally-limited spatial data available to parameterize runoff models.
The research presented in this paper addresses both limitations.
In both cases, the limitation factor is the surface tension, which restricts the particles size distribution from below.
Statistically significant associations were present between subgroups on change in activity limitation in both the unadjusted and adjusted analyses (Table 2).
The model pointed out that the major limitation in both studied systems is mass transfer limitation.
Growth of both diatoms in silica limitation did not induce changes in TAG levels, whereas nitrogen limitation induced an additional increase (almost 20%) in TAG productivity (19 μmol L−1 day−1 in T. weissflogii and 45 μmol L−1 day−1 in C. cryptica) in comparison with replete conditions.
In both cases, technological limitations have prevented scientists from studying these sounds in detail.
In this paper, we compare the results given by different codes and point out algorithmic limitations both in terms of physical accuracy and computational performances.
