Research:
Research Interests:
Deep cumulonimbus clouds form the upward branch of large scale thermal
circulations in the tropics. These circulations, which include the
global Hadley-Walker circulation and regional monsoon flows, are of
crucial importance not only to the tropics, but to mid-latitude
weather and climate as well. However, the mechanisms which control
the strength and location of these circulations are imperfectly
understood. Some of the biggest uncertainties are related to how
cumulus convection is controlled, and to the structure and vertical
transfer characteristics of this convection. The way in which water
vapor is vertically redistributed is an issue of particular concern.
Traveling tropical disturbances such as the Madden-Julian oscillation,
Kelvin waves, mixed Rossby-gravity waves, easterly waves, and tropical
storms are also very sensitive to cumulus convection.
My current interests are in unraveling how deep atmospheric convection
interacts with tropical circulations and how these circulations work
as a result. The TCS-08 project (see below) will provide insight into
this process in the context of developing and intensifying tropical
storms. In addition, we are using simple analytical models, numerical
models, including cumulus ensemble models, and a simplified large-scale
equatorial beta plane model, to test ideas about how convection works
in large scale tropical circulations. Ultimately, knowledge gained
from modeling, theory, and field observations should lead to better
representations of convection in numerical models, and hence better
weather and climate predictions. To this end we are also studying how
convection works in NCEP's Global Forecast System (GFS) model.
TPARC/TCS-08
In August and September of 2008 we will be participating in TCS-08, a
project to study the formation and structure change of western Pacific
typhoons. We will be based in Guam with excusions to Okinawa and
Japan as needed to follow the evolution of these typhoons. Two
aircraft will be based in Guam; the NRL P-3 aircraft with the ELDORA
Doppler radar, Doppler lidar, and dropsondes, as well as an Air Force
C-130 "hurricane hunter" deploying dropsondes. Other aircraft in this
project are the Taiwanese Dotstar jet and the German DLR Falcon. The
latter two aircraft, with help from the P-3 and the C-130, will study
the extratropical transition of west Pacific typhoons.
EPIC:
EPIC was a
program consisting of enhanced monitoring, modeling, and intensive
process studies designed to help us understand the coupled
ocean-atmosphere system of the east Pacific. EPIC was a part of the
U. S. CLIVAR Program with connections to other national programs in
Mexico, Central America, and South America. EPIC2001 was a process study
proposed under the umbrella of EPIC for a 6 week period in
September-October 2001 with the purpose of studying the east Pacific
intertropical convergence zone, the associated cross-equatorial
inflow, and the east Pacific warm pool. It also contained an
exploratory study of the ocean and atmosphere in the east Pacific
stratus region south of the equator. Read my personal view of EPIC's accomplishments.
Weak Temperature Gradient Cumulus Ensemble Model
The source code for the latest version of our weak temperature
gradient cumulus ensemble model is available here. It is in the form of a gzipped tar
file. The model is coded in the C language, and it needs a version of
MPI such as LAM/MPI to run, as well as
the Candis system.
Recent Papers and Preprints:
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Raymond, D. J., and Z. Fuchs, 2008:
Moisture modes and the Madden-Julian oscillation. Submitted to J. Climate.
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Raymond, D. J., and Z. Fuchs, 2007:
Convectively coupled gravity and moisture modes in a simple atmospheric model. Tellus, 59A, 627-640.
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Raymond, D. J., S. Sessions, and Z. Fuchs, 2007:
A theory for the spinup of tropical depressions.
Quarterly Journal of the Royal Meteorological Society, 133, 1743-1754.
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Raymond, D. J., 2007: Testing a cumulus
parameterization with a cumulus ensemble model in weak temperature
gradient mode.
Quarterly Journal of the Royal Meteorological Society, 133, 1073-1085.
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Fuchs, Z., and D. J. Raymond, 2007:
A simple, vertically resolved model of tropical disturbances with a
humidity closure. Tellus, 59A, 344-354.
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Raymond, D. J., and S. L. Sessions, 2007:
Evolution of convection during tropical cyclogenesis.
Geophys. Res. Lett., 34, L06811, doi:10.1029/2006GL028607.
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Raymond, D. J., C. S. Bretherton, and J. Molinari, 2006:
Dynamics of the intertropical convergence
zone of the East Pacific. J. Atmos. Sci., 63, 582-597.
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Fuchs, Z., and D. J. Raymond, 2005:
Large-scale modes in a rotating
atmosphere with radiative-convective instability and WISHE.
J. Atmos. Sci.,
62, 4084-4094.
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Lopez-Carillo, C., and D. J. Raymond, 2005:
Moisture tendency equations in a
tropical atmosphere.
J. Atmos. Sci.,
62, 1601-1613.
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Raymond, D. J., and X. Zeng, 2005:
Modelling tropical atmospheric
convection in the context of the weak temperature gradient
approximation. Quart. J. Roy. Meteor. Soc.,
131, 1301-1320.
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Raymond, D. J., S. K. Esbensen, C. Paulson, M. Gregg, C. S. Bretherton,
W. A. Petersen, R. Cifelli, L. K. Shay, C. Ohlmann, and P. Zuidema,
2004:
EPIC2001 and the coupled ocean-atmosphere
system of the tropical east Pacific.
Bull. Amer. Meteor. Soc.,
85, 1341-1354.
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Raymond, D. J., G. B. Raga, C. S. Bretherton, J. Molinari,
C. Lopez-Carrillo, and Z. Fuchs, 2003:
Convective forcing in the
intertropical convergence zone of the eastern Pacific.
J. Atmos. Sci.,
60, 2064-2082.
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Fuchs, Z., and D. J. Raymond, 2002:
Large-scale modes of a nonrotating
atmosphere with water vapor and cloud-radiation feedbacks.
J. Atmos. Sci.,
59, 1669-1679.
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Raymond, D. J., 2001:
A new model of the Madden-Julian
oscillation.
J. Atmos. Sci.,
58, 2807-2819.
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Raymond, D. J., 2000: The Hadley circulation as a radiative-convective
instability.
J. Atmos. Sci.,
57, 1286-1297.
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Raymond, D. J., 2000: Thermodynamic control
of tropical rainfall.
Quart. J. Roy. Meteor. Soc.,
126, 889-898.
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Raymond, D. J., and X. Zeng, 2000:
Instability and large-scale circulations in a two-column model of the tropical troposphere.
Quart. J. Roy. Meteor. Soc.,
126, 3117-3135.
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Raymond, D. J., C. Lopez-Carrillo, and L. Lopez Cavazos, 1998:
Case-studies of developing east Pacific easterly waves.
Quart. J. Roy. Meteor. Soc.,
124, 2005-2034.
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Raymond, D. J., and D. J. Torres, 1998: Fundamental moist modes of the
equatorial troposphere.
J. Atmos. Sci.,
55, 1771-1790.
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Wei, D., A. M. Blyth, and D. J. Raymond, 1998: Buoyancy of Convective
Clouds in TOGA COARE.
J. Atmos. Sci.,
55, 3381-3391.
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Jiang, H., and D. J. Raymond, 1995: Simulation of a mature mesoscale
convective system using a nonlinear balance model.
J. Atmos. Sci.,
52, 161-175.
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Raymond, D. J., 1995: Regulation of moist convection over the west
Pacific warm pool.
J. Atmos. Sci.,
52, 3945-3959.
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Raymond, D. J., and S. A. Lewis, 1995: Rotating convective disturbances
in the trades.
Quart. J. Roy. Meteor. Soc.,
121, 271-299.