However, this is essentially due to large scale dust storms that were common back then, compared to a lower level of
storminess now.
However, this is essentially due to large scale dust storms that were common back then, compared to a lower level of
storminess now.
Not exact matches
We suggest that recent coastal dune building from c.ad 1100 until
now, despite a sea level close to present and continuously rising, may be a direct consequence of the restoration of beaches after periods of recurrent
storminess.
It's not really obvious how all of this relates to the «variability» issue, but right
now I don't think we have a satisfactory handle on how mid-latitude
storminess might change in a new climate, in terms of frequency or intensity.