Physics
Scientific paper
Apr 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009georl..3607809r&link_type=abstract
Geophysical Research Letters, Volume 36, Issue 7, CiteID L07809
Physics
9
Atmospheric Processes: Convective Processes, Atmospheric Processes: Boundary Layer Processes, Atmospheric Processes: Precipitation (1854), Atmospheric Processes: Global Climate Models (1626, 4928)
Scientific paper
In most atmospheric circulation models used for climate projections, cloud and convective processes are not explicitly resolved but parameterized. Such models are known to produce a diurnal cycle of continental thunderstorms in phase with insolation, while observed precipitation peaks in late afternoon. We propose a new approach which corrects this long standing bias of parameterized convection. In this approach, deep convection triggering and intensity are controlled by sub-cloud processes: here boundary layer thermals and gust fronts, and potentially orography or surface heterogeneities. The representation of the diurnal cycle of deep convection is greatly improved in 1D mode, with rainfall maximum delayed from midday to late afternoon, provided parameterizations account for the key role played by shallow cumulus in preconditioning deep convection and by gust fronts in the self-sustaining of thunderstorms in the afternoon.
Grandpeix J. Y.
Hourdin Fréderic
Lafore J. P.
Rio C.
No associations
LandOfFree
Shifting the diurnal cycle of parameterized deep convection over land does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Shifting the diurnal cycle of parameterized deep convection over land, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Shifting the diurnal cycle of parameterized deep convection over land will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1521656