Extreme Rainfall Mechanisms Exhibited by Typhoon Morakot (2009)
Terrestrial, Atmospheric and Oceanic Sciences, 2011 Moderate Typhoon Morakot (2009) became the most catastrophic typhoon in Taiwan on record. The MM5 numerical experiments with and without bogus data assimilation (BDA) were used to investigate the extreme rainfall mechanisms in Taiwan associated with the ...
Ching-Yuang Huang +2 more
doaj +1 more source
, 2014 This work reports a high spatial resolution observations toward Orion KL region with high critical density lines of CH$_{3}$CN (12$_{4}$-11$_{4}$) and CH$_{3}$OH (8$_{-1, 8}$-7$_{0, 7}$) as well as continuum at $\sim$1.3 mm band.
Liu, Tie, Qin, Sheng-Li, Wu, Yuefang
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Meteorological Applications, Volume 32, Issue 6, November/December 2025.Higher Turbulent Kinetic Energy in YSU indicates strong turbulence in the boundary layer (thick black curved arrows) resulting in the exchange of turbulent fluxes to the upper atmosphere through strong updrafts (Red arrows), making the atmosphere saturated, aiding the realistic prediction of rainfall associated with thunderstorms compared to MYJ and ...
Kesireddy Lakshman +4 more
wiley +1 more source
The subtropical global plume in the Pacific Exploratory Mission-Tropics A (PEM-Tropics A), PEM-Tropics B, and the Global Atmospheric Sampling Program (GASP): How tropical emissions affect the remote Pacific [PDF]
, 2002 [1] An extended southern subtropical plume of CO meanders>15,000 km around the world, gradually spreading around 20 S. This southern pollution plume is most noticeable in the burning season, southern spring; a similar subtropical plume appears in the ...
Blake, DR +4 more
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Influences of Asymmetric Heating on Hurricane Evolution in the MM5
Journal of the Atmospheric Sciences, 2005 Abstract While previous idealized studies have demonstrated the importance of asymmetric atmospheric features in the intensification of a symmetric tropical cyclone vortex, the role of convectively generated asymmetries in creating changes in the azimuthally averaged cyclone is not well understood.
Lloyd J. Shapiro, J. Dominique Möller
openaire +1 more source
A Review of Drivers of Cool Season Rainfall in Southwest Western Australia
WIREs Climate Change, Volume 16, Issue 6, November/December 2025.Schematic of weather systems and larger‐scale climate drivers that influence South West Western Australia (SWWA) winter rainfall during (a) a typical dry SWWA winter, and (b) a typical wet SWWA winter, where SWWA is depicted by the green shaded area, the “H” in (a) illustrates the influence of high‐pressure in directing dry continental easterly wind ...
Kerryn A. Hawke +2 more
wiley +1 more source
Análise Comparativa das Simulações do Modelo de Mesoescala MM5 e Dados Meteorológicos Observados para a Região do Galeão/RJ. [PDF]
Anuário do Instituto de Geociências, 2006 The main objective of this study is to analyze the MM5 MesoscaleModel results comparing with observational datasets in surface and altitude from meteorological station of Galeão International Airport- RIO DE JANEIRO.
Eduardo Barbosa Corrêa +2 more
doaj
Using Bayesian Model Averaging (BMA) to calibrate probabilistic surface temperature forecasts over Iran [PDF]
Annales Geophysicae, 2011 Using Bayesian Model Averaging (BMA), an attempt was made to obtain calibrated probabilistic numerical forecasts of 2-m temperature over Iran. The ensemble employs three limited area models (WRF, MM5 and HRM), with WRF used with five different ...
I. Soltanzadeh, M. Azadi, G. A. Vakili
doaj +1 more source
Investigate the impacts of assimilating satellite rainfall estimates on rainstorm forecast over southwest United States [PDF]
, 2004 Using the MM5-4DVAR system, a monsoon rainstorm case over southern Arizona (5-6 August 2002) was investigated for the influence of assimilating satellite rainfall estimates on precipitation forecasts.
Gao, X, Sorooshian, S, Xiao, Q, Xu, J
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Dynamics of wind-driven upwelling and relaxation between Monterey Bay and Point Arena: Local-, regional-, and gyre-scale controls [PDF]
, 2009 In north and central California, equatorward winds drive equatorward flows and the upwelling of cold dense water over the shelf during the midspring and summer upwelling season.
Dever, Edward P, Pringle, James M.
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