Difference between revisions of "Cloud convection"

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== Overview ==
 
== Overview ==
  
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From Section 2.10 of ''Wu et al'' [2007]:
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From Section 2, paragraph 10 of ''Wu et al'' [2007]:
  
 
<blockquote>A major difference between the GEOS-3, GEOS-4, and GISS models is the treatment of wet convection.  GEOS-3 [and now also GEOS-5, ''ed.''] uses the Relaxed Arakawa-Schubert convection scheme [''Moorthi and Suarez'', 1992]. GEOS-4 has separate treatments of deep and shallow convection following the schemes developed by ''Zhang and McFarlane'' [1995] and ''Hack'' [1994]. The convection scheme in the GISS GCM was described by ''Del Genio and Yao'' [1993]. Unlike the GEOS models, the GISS GCM allows for condensed water in the atmosphere (i.e., condensed water is not immediately precipitated), resulting in frequent nonprecipitating shallow convection. In the wet deposition scheme, we do not scavenge soluble species from shallow convective updrafts at altitudes lower than 700 hPa in the GISS-driven model, whereas we do in the GEOS-driven model [''Liu et al.'', 2001].</blockquote>
 
<blockquote>A major difference between the GEOS-3, GEOS-4, and GISS models is the treatment of wet convection.  GEOS-3 [and now also GEOS-5, ''ed.''] uses the Relaxed Arakawa-Schubert convection scheme [''Moorthi and Suarez'', 1992]. GEOS-4 has separate treatments of deep and shallow convection following the schemes developed by ''Zhang and McFarlane'' [1995] and ''Hack'' [1994]. The convection scheme in the GISS GCM was described by ''Del Genio and Yao'' [1993]. Unlike the GEOS models, the GISS GCM allows for condensed water in the atmosphere (i.e., condensed water is not immediately precipitated), resulting in frequent nonprecipitating shallow convection. In the wet deposition scheme, we do not scavenge soluble species from shallow convective updrafts at altitudes lower than 700 hPa in the GISS-driven model, whereas we do in the GEOS-driven model [''Liu et al.'', 2001].</blockquote>

Revision as of 21:42, 19 February 2010

Overview

From Section 2, paragraph 10 of Wu et al [2007]:

A major difference between the GEOS-3, GEOS-4, and GISS models is the treatment of wet convection. GEOS-3 [and now also GEOS-5, ed.] uses the Relaxed Arakawa-Schubert convection scheme [Moorthi and Suarez, 1992]. GEOS-4 has separate treatments of deep and shallow convection following the schemes developed by Zhang and McFarlane [1995] and Hack [1994]. The convection scheme in the GISS GCM was described by Del Genio and Yao [1993]. Unlike the GEOS models, the GISS GCM allows for condensed water in the atmosphere (i.e., condensed water is not immediately precipitated), resulting in frequent nonprecipitating shallow convection. In the wet deposition scheme, we do not scavenge soluble species from shallow convective updrafts at altitudes lower than 700 hPa in the GISS-driven model, whereas we do in the GEOS-driven model [Liu et al., 2001].

Updraft scavenging of soluble tracers (as applied to both the Relaxed Arakawa and Hack/Zhang-McFarlane schemes in GEOS-Chem) is described in Section 1 of Jacob et al, 2000.

--Bob Y. 13:13, 19 February 2010 (EST)

Relaxed Arakawa-Schubert scheme

This is the convection scheme that GEOS-Chem uses with both GEOS-3 and GEOS-5 meteorology. The source code for this scheme is located in routine NFCLDMX in convection_mod.f.

Hack and Zhang-McFarlane schemes

This is the convection scheme that GEOS-Chem uses with both GEOS-4 and GCAP meteorology.

GEOS-4

The source code for the convection scheme required for GEOS-4 meteorology is contained within the F90 module fvdas_convect_mod.f. The main driver is called FVDAS_CONVECT. This routine calls the following routines:

  1. ARCONVTRAN: Prepares arrays for use by CONVTRAN
  2. CONVTRAN: Main driver for deep convection (i.e. Zhang/McFarlane scheme)
  3. HACK_CONV: Main driver for shallow convection (i.e. Hack scheme)

GISS

The source code for the convection scheme required for GISS/GCAP meteorology is contained within the F90 module gcap_convect_mod.f. The main driver is called GCAP_CONVECT. This routine calls the following routines:

  1. ARCONVTRAN: Prepares arrays for use by CONVTRAN
  2. CONVTRAN: Main driver for deep convection (i.e. Zhang/McFarlane scheme)

There is no equivalent routine to HACK_CONV for the GCAP meterology. Instead, ARCONVTRAN and CONVTRAN are called with entraining mass fluxes, and then again with non-entraining mass fluxes.

--Bob Y. 13:11, 19 February 2010 (EST)

Validation

See Bey et al [2001], Liu et al [2001], and Wu et al [2007].

References

  1. Allen, D.J, R.B. Rood, A.M. Thompson, and R.D. Hidson, Three dimensional 222Rn calculations using assimilated data and a convective mixing algorithm, J. Geophys. Res, 101, 6871-6881, 1986a.
  2. Allen, D.J. et al, Transport induced interannual variability of carbon monoxide using a chemistry and transport model, 101, J. Geophys. Res, 28,655-28-670, 1986b.
  3. Bey I., D. J. Jacob, R. M. Yantosca, J. A. Logan, B. Field, A. M. Fiore, Q. Li, H. Liu, L. J. Mickley, and M. Schultz, Global modeling of tropospheric chemistry with assimilated meteorology: Model description and evaluation, J. Geophys. Res., 106, 23,073-23,096, 2001. PDF
  4. Del Genio, A. D., and M. Yao, Efficient cumulus parameterization for long-term climate studies: The GISS scheme, in The Representation of Cumulus Convection in Numerical Models, Meteorol. Monogr., 46, 181–184, 1993.
  5. Hack, J.J., Parameterization of moist convection in the National Center for Atmospheric Research Community Climate Model (CCM2), <u<J. Geophys. Res.</u>, 99, 5551–5568, 1994.
  6. Jacob, D.J. H. Liu, C.Mari, and R.M. Yantosca, Harvard wet deposition scheme for GMI, Harvard University Atmospheric Chemistry Modeling Group, revised March 2000.
  7. Liu, H., et al. (2001), Constraints from 210Pb and 7Be on wet deposition and transport in a global three-dimensional chemical tracer model driven by assimilated meteorological fields, J. Geophys. Res., 106, 12,109–12,128. PDF
  8. Moorthi, S., and M. J. Suarez, Relaxed Arakawa-Schubert: A parameterization of moist convection for general circulation models, Mon. Weather Rev., 120, 978– 1002, 1992.
  9. Wu, S., L.J. Mickley, D.J. Jacob, J.A. Logan, R.M. Yantosca, and D. Rind, Why are there large differences between models in global budgets of tropospheric ozone?, J. Geophys. Res., 112, D05302, doi:10.1029/2006JD007801, 2007. PDF
  10. Zhang, G. J., and N. A. McFarlane, Sensitivity of climate simulations to the parameterization of cumulus convection in the Canadian Climate Centre general circulation model, Atmos. Ocean, 33(3), 407–446, 1995.

--Bob Y. 13:11, 19 February 2010 (EST)

Known issues

None at this time.

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