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technique O
for O
precipitation B-climate-nature
suitable O
for O
complex O
topography B-climate-nature
. O
The O
daily O
evolution O
and O
the O
annual O
cycleof O
precipitation B-climate-nature
in O
WRFERA B-climate-models
closely O
reproduces O
the O
observations O
. O
Conversely O
, O
WRFCESM B-climate-models
shows O
a O
different O
seasonality O
with O
peak O
precipitation B-climate-nature
in O
winter O
and O
not O
in O
summer O
as O
in O
the O
observations O
or O
in O
WRF B-climate-models
- I-climate-models
ERA I-climate-models
. O
-DOCSTART- -X- O O186a36dc5c5e7ce30bb8ae0865f15fcb
Over O
recent O
decades O
it O
has O
become O
clear O
that O
the O
middle B-climate-nature
atmosphere I-climate-nature
has O
a O
significant O
impact O
on O
surface B-climate-nature
and O
tropospheric B-climate-nature
climate O
. O
A O
better O
understanding O
of O
the O
middle B-climate-nature
atmosphere I-climate-nature
and O
how O
it O
reacts O
to O
the O
current O
increase O
in O
the O
concentration B-climate-properties
of O
carbon B-climate-greenhouse-gases
dioxide I-climate-greenhouse-gases
( O
CO2 B-climate-greenhouse-gases
) O