David J. Raymond mainly investigates Convection, Environmental science, Climatology, Atmospheric sciences and Vorticity. His research is interdisciplinary, bridging the disciplines of Troposphere and Convection. His Climatology research focuses on subjects like Madden–Julian oscillation, which are linked to Intertropical Convergence Zone.
He has researched Atmospheric sciences in several fields, including Latent heat and Temperature gradient. His research integrates issues of Classical mechanics, Mathematical analysis and Rossby number in his study of Vorticity. His Convective instability research incorporates themes from Thunderstorm, Potential vorticity, Free convective layer and Mesoscale meteorology.
His primary areas of study are Convection, Atmospheric sciences, Environmental science, Climatology and Meteorology. His work on Convective instability and Atmospheric convection is typically connected to Convective inhibition as part of general Convection study, connecting several disciplines of science. His Atmospheric sciences study integrates concerns from other disciplines, such as Moisture, Sea surface temperature, Precipitation and Free convective layer.
The Climatology study combines topics in areas such as Madden–Julian oscillation, Intertropical Convergence Zone and Vorticity. His study in Intertropical Convergence Zone is interdisciplinary in nature, drawing from both Equator and Tropical wave. As part of one scientific family, he deals mainly with the area of Mechanics, narrowing it down to issues related to the Kelvin wave, and often Beta plane.
Convection, Madden–Julian oscillation, Environmental science, Climatology and Atmospheric sciences are his primary areas of study. In general Convection study, his work on Atmospheric convection often relates to the realm of High resolution, thereby connecting several areas of interest. His studies in Madden–Julian oscillation integrate themes in fields like Quantum electrodynamics, Oceanography and Statistical physics.
His Climatology research is multidisciplinary, incorporating perspectives in Convective instability, Instability and Precipitation. When carried out as part of a general Atmospheric sciences research project, his work on Troposphere and Rossby wave is frequently linked to work in Convective inhibition and Mode, therefore connecting diverse disciplines of study. The study incorporates disciplines such as Quasistatic process and Potential vorticity, Vorticity in addition to Moisture.
David J. Raymond mostly deals with Convection, Atmospheric sciences, Climatology, Environmental science and Rossby wave. His Convection study focuses on Atmospheric convection in particular. His Atmospheric sciences research focuses on Precipitation and how it connects with Kelvin wave and Radiosonde.
His Climatology research incorporates themes from Madden–Julian oscillation and Convective instability. His work in Environmental science incorporates the disciplines of Moisture and Storm. The concepts of his Rossby wave study are interwoven with issues in Mechanics and Instability.
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The Representation of Cumulus Convection in Numerical Models
Kerry A. Emanuel;David J. Raymond.
(1993)
A Theory for Long-Lived Mesoscale Convective Systems
D. J. Raymond;H. Jiang.
Journal of the Atmospheric Sciences (1990)
A New Model of the Madden–Julian Oscillation
David J. Raymond.
Journal of the Atmospheric Sciences (2001)
Regulation of moist convection over the West Pacific warm pool
David J. Raymond.
Journal of the Atmospheric Sciences (1995)
A Stochastic Mixing Model for Nonprecipitating Cumulus Clouds
David J. Raymond;Alan M. Blyth.
Journal of the Atmospheric Sciences (1986)
The Mechanics of Gross Moist Stability
David J Raymond;Sharon L Sessions;Adam H Sobel;Željka Fuchs.
Journal of Advances in Modeling Earth Systems (2009)
Moisture modes and the Madden-Julian oscillation.
David J. Raymond;Željka Fuchs.
Journal of Climate (2009)
Nonlinear Balance and Potential‐Vorticity Thinking At Large Rossby Number
D. J. Raymond.
Quarterly Journal of the Royal Meteorological Society (1992)
Thermodynamic control of tropical rainfall
D. J. Raymond.
Quarterly Journal of the Royal Meteorological Society (2000)
Modelling tropical atmospheric convection in the context of the weak temperature gradient approximation
David J. Raymond;Xiping Zeng.
Quarterly Journal of the Royal Meteorological Society (2005)
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