Assimilation of Satellite Data in Improving Numerical Simulation of Tropical Cyclones: Progress, Challenge and Development

2009 ◽  
pp. 163-176 ◽  
Author(s):  
Zhaoxia Pu
Keyword(s):  
Numerical Simulation ◽  
Tropical Cyclones ◽  
Satellite Data

Ionospheric precursors of the intensification of isolated tropical cyclones according to the IKB-1300 and Cosmos-1809 satellite data

2015 ◽  
Vol 55 (2) ◽  
pp. 246-260 ◽  
Author(s):  
V. M. Kostin ◽  
G. G. Belyaev ◽  
B. Boichev ◽  
E. P. Trushkina ◽  
O. Ya. Ovcharenko
Keyword(s):  
Tropical Cyclones ◽  
Satellite Data

scholarly journals Influence of frontal cyclone evolution on the 2009 (Ekman) and 2010 (Franklin) Loop Current eddy detachment events

Ocean Science ◽  
2014 ◽  
Vol 10 (6) ◽  
pp. 947-965 ◽  
Author(s):  
Y. S. Androulidakis ◽  
V. H. Kourafalou ◽  
M. Le Hénaff
Keyword(s):  
Numerical Simulation ◽  
Gulf Of Mexico ◽  
Satellite Data ◽  
Potential Vorticity ◽  
In Situ Measurements ◽  
Loop Current ◽  
Positive Potential ◽  
Eastern Gulf Of Mexico ◽  
And Migration

Abstract. The anticyclonic Loop Current Eddy (LCE) shedding events are strongly associated with the evolution of Loop Current Frontal Eddies (LCFEs) over the eastern Gulf of Mexico (GoM). A numerical simulation, in tandem with in situ measurements and satellite data, was used to investigate the Loop Current (LC) evolution and the surrounding LCFE formation, structure, growth and migration during the Eddy Ekman and Eddy Franklin shedding events in the summers of 2009 and 2010, respectively. During both events, northern GoM LCFEs appeared vertically coherent to at least 1500 m in temperature observations. They propagated towards the base of the LC, where, together with the migration of Campeche Bank (southwest GoM shelf) eddies from south of the LC, contributed to its "necking-down". Growth of Campeche Bank LCFEs involved in Eddy Franklin was partially attributed to Campeche Bank waters following upwelling events. Slope processes associated with such upwelling included offshore exports of high positive potential vorticity that may trigger cyclone formation and growth. The advection and growth of LCFEs, originating from the northern and southern GoM, and their interaction with the LC over the LCE detachment area favor shedding conditions and may contribute to the final separation of the LCE.

scholarly journals Ionosphere Parameters Changing by Interactive Tropical Cyclones according to Cosmos-1809 and Intercosmos Bulgaria-1300 Satellite Data

2018 ◽  
Author(s):  
B. Boychev ◽  
G. Belyaev ◽  
V. Kostin ◽  
O. Ovcharenko ◽  
E. Trushkina
Keyword(s):  
Tropical Cyclones ◽  
Satellite Data

Calculation of Pressure in Tropical Cyclones Using Satellite Data

2019 ◽  
Vol 44 (9) ◽  
pp. 588-593
Author(s):  
A. S. Eremenko ◽  
V. A. Kachur
Keyword(s):  
Tropical Cyclones ◽  
Satellite Data

scholarly journals Meteorological Education and Training Using A-Train Profilers

2012 ◽  
Vol 93 (5) ◽  
pp. 687-696 ◽  
Author(s):  
Thomas F. Lee ◽  
Richard L. Bankert ◽  
Cristian Mitrescu
Keyword(s):  
Tropical Cyclones ◽  
Satellite Data ◽  
Satellite Images ◽  
Satellite Observations ◽  
Two Dimensional ◽  
Marine Stratocumulus ◽  
Severe Thunderstorm ◽  
Fundamental Information ◽  
Frontal Systems ◽  
And Training

NASA A-Train vertical profilers provide detailed observations of atmospheric features not seen in traditional imagery from other weather satellite data. CloudSat and Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) profiles vividly depict the vertical dimension of otherwise two-dimensional features shown in mapped products. However, most forecasters have never seen these profiles and do not appreciate their capacity to convey fundamental information about cloud and precipitation systems. Here, these profiles are accompanied by weather satellite images and explained in the context of various meteorological regimes. Profile examples are shown over frontal systems, marine stratocumulus, orographic barriers, tropical cyclones, and a severe thunderstorm.

Impact of period and timescale of FDDA analysis nudging on the numerical simulation of tropical cyclones in the Bay of Bengal

2014 ◽  
Vol 74 (3) ◽  
pp. 2109-2128 ◽  
Author(s):  
V. Yesubabu ◽  
C. V. Srinivas ◽  
S. S. V. S. Ramakrishna ◽  
K. B. R. R. Hari Prasad
Keyword(s):  
Numerical Simulation ◽  
Tropical Cyclones ◽  
Bay Of Bengal
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