Academic literature on the topic 'Cyclones'

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Journal articles on the topic "Cyclones"

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Scherrmann, Alexander, Heini Wernli, and Emmanouil Flaounas. "Origin of low-tropospheric potential vorticity in Mediterranean cyclones." Weather and Climate Dynamics 4, no. 1 (January 25, 2023): 157–73. http://dx.doi.org/10.5194/wcd-4-157-2023.

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Abstract. Mediterranean cyclones are extratropical cyclones, typically of smaller size and weaker intensity than other cyclones that develop over the main open ocean storm tracks. Nevertheless, Mediterranean cyclones can attain high intensities, even comparable to the ones of tropical cyclones, and thus cause large socioeconomic impacts in the densely populated coasts of the region. After cyclogenesis takes place, a large variety of processes are involved in the cyclone’s development, contributing with positive and negative potential vorticity (PV) changes to the lower-tropospheric PV anomalies in the cyclone center. Although the diabatic processes that produce these PV anomalies in Mediterranean cyclones are known, it is still an open question whether they occur locally within the cyclone itself or remotely in the environment (e.g., near high orography) with a subsequent transport of high-PV air into the cyclone center. This study introduces a Lagrangian method to determine the origin of the lower-tropospheric PV anomaly, which is applied climatologically to ERA5 reanalysis and to 12 monthly simulations, performed with the integrated forecasting system (IFS) model. We define and quantify so-called “cyclonic” and “environmental” PV and find that the main part of the lower-tropospheric PV anomaly (60 %) is produced within the cyclone, shortly prior (−12 h) to the cyclones' mature stage. Nevertheless, in 19.5 % of the cyclones the environmental PV production near the mountains surrounding the Mediterranean Basin plays a significant role in forming the low-tropospheric PV anomaly and therefore in determining the intensity of these cyclones. The analysis of PV tendencies from the IFS simulations reveals that the major PV production inside the cyclone is typically due to convection and microphysics, whereas convection and turbulent momentum tendencies cause most of the positive PV changes in the environment.
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Oruba, Ludivine, Guillaume Lapeyre, and Gwendal Rivière. "On the Northward Motion of Midlatitude Cyclones in a Barotropic Meandering Jet." Journal of the Atmospheric Sciences 69, no. 6 (June 1, 2012): 1793–810. http://dx.doi.org/10.1175/jas-d-11-0267.1.

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Abstract The combined effects of the deformation (horizontal stretching and shearing) and nonlinearities on the beta drift of midlatitude cyclones are studied using a barotropic quasigeostrophic model on the beta plane. It is found that, without any background flow, a cyclonic vortex moves more rapidly northward when it is initially strongly stretched along a mostly north–south direction. This meridional stretching is more efficient at forming an anticyclone to the east of the cyclone through Rossby wave radiation. The cyclone–anticyclone couple then forms a nonlinear vortex dipole that propagates mostly northward. The case of a cyclone embedded in uniformly sheared zonal flows is then studied. A cyclone evolving in an anticyclonic shear is stretched more strongly, develops a stronger anticyclone, and moves faster northward than a cyclone embedded in a cyclonic shear, which remains almost isotropic. Similar results are found in the general case of uniformly sheared nonzonal flows. The evolution of cyclones is also investigated in the case of a more realistic meandering jet whose relative vorticity gradient creates an effective beta and whose deformation field is spatially varying. A statistical study reveals a strong correlation among the cyclone’s stretching, the anticyclone strength, and the velocity toward the jet center. These different observations agree with the more idealized cases. Finally, these results provide a rationale for the existence of preferential zones for the jet-crossing phase: that is, the phase when a cyclone crosses a jet from its anticyclonic to its cyclonic side.
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Chaudhuri, Sutapa, and Anindita De Sarkar. "Severity of Tropical Cyclones atypical during El Nino – A Statistical Elucidation." Asian Journal of Water, Environment and Pollution 6, no. 4 (January 2009): 79–85. http://dx.doi.org/10.3233/ajw-2009-6_4_11.

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Tropical cyclones are one of nature's most violent manifestations and potentially the deadliest of all meteorological phenomena. The casualty associated with major cyclones in the Indian sub-continent gives an idea about its enormous destructive capability. The effect of El Nino over Indian Ocean is not fully understood yet. The present study is an attempt to establish a relationship between El Nino and severity of tropical cyclones. The rationale of the present study is to view whether a persistent cyclonic disturbance leads to the development of a tropical cyclone or severe tropical cyclone during an El Nino year. Statistical techniques are adopted to attain the objectives. The results of the study reveal that in the El Nino year cyclonic disturbances may turn to tropical cyclones but turning to its severity is absolutely unusual.
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Binder, Hanin, Maxi Boettcher, Hanna Joos, and Heini Wernli. "The Role of Warm Conveyor Belts for the Intensification of Extratropical Cyclones in Northern Hemisphere Winter." Journal of the Atmospheric Sciences 73, no. 10 (September 21, 2016): 3997–4020. http://dx.doi.org/10.1175/jas-d-15-0302.1.

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Abstract The role of warm conveyor belts (WCBs) and their associated positive low-level potential vorticity (PV) anomalies are investigated for extratropical cyclones in Northern Hemisphere winter, using ERA-Interim and composite techniques. The Spearman correlation coefficient of 0.68 implies a moderate to strong correlation between cyclone intensification and WCB strength. Hereby, cyclone intensification is quantified by the normalized maximum 24-h central sea level pressure deepening and WCB strength by the WCB air mass associated with the cyclone’s 24-h period of strongest deepening. Explosively intensifying cyclones typically have strong WCBs and pronounced WCB-related PV production in the cyclone center; they are associated with a WCB of type W2, which ascends close to the cyclone center. Cyclones with similar WCB strength but weak intensification are either diabatic Rossby waves, which do not interact with an upper-level disturbance, or cyclones where much of the WCB-related PV production occurs far from the cyclone center and thereby does not contribute strongly to cyclone deepening (WCB of type W1, which ascends mainly along the cold front). The category of explosively intensifying cyclones with weak WCBs is inhomogeneous but often characterized by a very low tropopause or latent heating independent of WCBs. These findings reveal that (i) diabatic PV production in WCBs is essential for the intensification of many explosive cyclones, (ii) the importance of WCBs for cyclone development strongly depends on the location of the PV production relative to the cyclone center, and (iii) a minority of explosive cyclones is not associated with WCBs.
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Dacre, H. F., O. Martínez-Alvarado, and C. O. Mbengue. "Linking Atmospheric Rivers and Warm Conveyor Belt Airflows." Journal of Hydrometeorology 20, no. 6 (June 1, 2019): 1183–96. http://dx.doi.org/10.1175/jhm-d-18-0175.1.

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Abstract Extreme precipitation associated with extratropical cyclones can lead to flooding if cyclones track over land. However, the dynamical mechanisms by which moist air is transported into cyclones is poorly understood. In this paper we analyze airflows within a climatology of cyclones in order to understand how cyclones redistribute moisture stored in the atmosphere. This analysis shows that within a cyclone’s warm sector the cyclone-relative airflow is rearwards relative to the cyclone propagation direction. This low-level airflow (termed the feeder airstream) slows down when it reaches the cold front, resulting in moisture flux convergence and the formation of a band of high moisture content. One branch of the feeder airstream turns toward the cyclone center, supplying moisture to the base of the warm conveyor belt where it ascends and precipitation forms. The other branch turns away from the cyclone center exporting moisture from the cyclone. As the cyclone travels, this export results in a filament of high moisture content marking the track of the cyclone (often used to identify atmospheric rivers). We find that both cyclone precipitation and water vapor transport increase when moisture in the feeder airstream increases, thus explaining the link between atmospheric rivers and the precipitation associated with warm conveyor belt ascent. Atmospheric moisture budgets calculated as cyclones pass over fixed domains relative to the cyclone tracks show that continuous evaporation of moisture in the precyclone environment moistens the feeder airstream. Evaporation behind the cold front acts to moisten the atmosphere in the wake of the cyclone passage, potentially preconditioning the environment for subsequent cyclone development.
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Zy Misa Harivelo, Rakotoarimanana, Rakotoarimanana Zy Harifidy, Pandin Moses Glorino Rumambo, and Waloejo Christrijogo Sumartono. "Analysis of tropical cyclones 2000-2020 in Madagascar." Disaster Advances 15, no. 3 (February 25, 2022): 13–20. http://dx.doi.org/10.25303/1503da1320.

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Madagascar is among the ten countries most exposed to cyclonic disasters in the world due to its geographical position. The country faces serious problems directly related to tropical cyclones every year. This research aims to analyze the cyclones in Madagascar from 2000 to 2020 focusing on the impact of the cyclone based on human losses and costs. The findings showed that during the past 20 years, 39 significant cyclones have affected Madagascar. On an average, 02 cyclones per year hit the country but its frequency has been decreasing since 2014. Cyclone Eline, Gafilo and Ivan were considered the most dangerous and have caused serious damages to the country. The number of victims caused by the cyclone, Eline, in 2000 were numerous while the cyclone Ivan in 2008 led many people to homelessness. In addition, the cyclone Gafilo in 2004 was recorded as the deadliest, costliest and has provoked many injuries including missing people. The number of victims, homeless, injured, missing and the cost of damage increase depending on the intensity of the cyclone. The East, North-East, West and Southwest coasts are most often hit by cyclones. Despite the frequency and damage of cyclones in the country, the actions carried out to reduce or mitigate the impacts of cyclones are still not sustainable, which makes the populations more vulnerable.
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Knowland, K. Emma, Ruth M. Doherty, Kevin I. Hodges, and Lesley E. Ott. "The influence of mid-latitude cyclones on European background surface ozone." Atmospheric Chemistry and Physics 17, no. 20 (October 19, 2017): 12421–47. http://dx.doi.org/10.5194/acp-17-12421-2017.

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Abstract. The relationship between springtime mid-latitude cyclones and background ozone (O3) is explored using a combination of observational and reanalysis data sets. First, the relationship between surface O3 observations at two rural monitoring sites on the west coast of Europe – Mace Head, Ireland, and Monte Velho, Portugal – and cyclone track frequency in the surrounding regions is examined. Second, detailed case study examination of four individual mid-latitude cyclones and the influence of the associated frontal passage on surface O3 is performed. Cyclone tracks have a greater influence on the O3 measurements at the more northern coastal European station, Mace Head, located within the main North Atlantic (NA) storm track. In particular, when cyclones track north of 53° N, there is a significant relationship with high levels of surface O3 (> 75th percentile). The further away a cyclone is from the NA storm track, the more likely it will be associated with both high and low (< 25th percentile) levels of O3 at the observation site during the cyclone's life cycle. The results of the four case studies demonstrate (a) the importance of the passage of a cyclone's cold front in relation to surface O3 measurements, (b) the ability of mid-latitude cyclones to bring down high levels of O3 from the stratosphere, and (c) that accompanying surface high-pressure systems and their associated transport pathways play an important role in the temporal variability of surface O3. The main source of high O3 to these two sites in springtime is from the stratosphere, either from direct injection into the cyclone or associated with aged airstreams from decaying downstream cyclones that can become entrained and descend toward the surface within new cyclones over the NA region.
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Rudeva, Irina, and Sergey K. Gulev. "Composite Analysis of North Atlantic Extratropical Cyclones in NCEP–NCAR Reanalysis Data." Monthly Weather Review 139, no. 5 (May 2011): 1419–46. http://dx.doi.org/10.1175/2010mwr3294.1.

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Composite analysis of North Atlantic midlatitudinal winter cyclones is performed using NCEP–NCAR reanalysis data for the 60-yr period from 1948 to 2007. The composites were developed using an advanced methodology involving the coordinate transform of cyclones into a nondimensional azimuthal coordinate system and the further collocation of fields. Composite analysis is performed for air–sea turbulent fluxes, heat content, precipitable water, and precipitation for 576 oceanic cyclones generated in the Gulf Stream area in winter (January–March) from 1948 to 2007. For the region of cyclone generation over the Gulf Stream, composites were analyzed for different cyclone intensities. Over the whole North Atlantic, composites were developed throughout the life cycle and for different cyclone types classified by the regions of their migration. These classifications allow the case-to-case variability to be minimized and the robustness of the composite to be boosted. In the region of cyclone generation over the Gulf Stream, characteristics of the composites strongly depend on the cyclone intensity quantified through the radial sea level pressure difference between the cyclone’s edge and its center. Stronger cyclone intensity implies larger turbulent fluxes in the rear of a cyclone and stronger precipitation in the forward part. Cyclones gradually dry with the water content and precipitation rate decreasing by about 40% and 50%–70%, respectively, during the lifetime. Although composites of air–sea turbulent fluxes show locally very strong positive fluxes in the rear part of the cyclone, the total air–sea turbulent fluxes provided by cyclones are not significantly different from the averaged background fluxes. This shows that the formation of extreme air–sea fluxes by cyclones is connected to the larger-scale circulation conditions, particularly to the cyclone–anticyclone transition zones.
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Sahoo, Umesh Chandra, Suresh Ranjan Dash, and Chandra Sekhar Sahu. "Climate-resilient road design in coastal areas subjected to cyclones and associated floods." Infrastructure Asset Management 8, no. 4 (December 1, 2021): 209–18. http://dx.doi.org/10.1680/jinam.21.00010.

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Cyclones and the associated floods have recently become a regular problem for many states of India, particularly on its west and east coasts. Odisha (renamed from Orissa in 2011) is a state located along the eastern coast of India that experiences tropical cyclones mainly from the Bay of Bengal. Some of the recent severe cyclonic storms that caused large-scale devastation in Odisha in the last decade include cyclone Amphan in May 2020, cyclone Fani in May 2019, cyclone Titli in October 2018, cyclone Hudhud in October 2014 and cyclone Phailin in October 2013. The roads, being one of the essential lifeline infrastructure facilities, commonly get damaged during these cyclonic floods in terms of floodwater overtopping, erosion of road surfaces, shoulders and embankment slopes, and even the washing out of the whole roadway section. These recent events have indicated that special attention is needed to minimise damage to this vital lifeline infrastructure by developing and adopting climate-resilient road infrastructure. This paper focuses on the damage assessment of transportation infrastructure during the recent cyclones and associated floods in Odisha, and advances some recommendations for possible measures to be taken for the design of cyclone- and flood-resilient road infrastructure.
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Lim, Eun-Pa, and Ian Simmonds. "Southern Hemisphere Winter Extratropical Cyclone Characteristics and Vertical Organization Observed with the ERA-40 Data in 1979–2001." Journal of Climate 20, no. 11 (June 1, 2007): 2675–90. http://dx.doi.org/10.1175/jcli4135.1.

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Abstract The mean characteristics and trends of Southern Hemisphere (SH) winter extratropical cyclones occurring at six levels of the troposphere over the period 1979–2001 have been investigated using the 40-yr ECMWF Re-Analysis (ERA-40) data. Cyclonic systems were identified with the Melbourne University cyclone finding and tracking scheme. This study shows that mean sea level pressure (MSLP) cyclones are more numerous, more intense, smaller, deeper, and slower moving than higher-level cyclones. The novel vertical tracing scheme devised for this research revealed that about 52% of SH winter MSLP cyclones have a vertically well organized structure, extending through to the 500-hPa level. About 80% of these vertically coherent SH cyclones keep their westward tilt until the surface cyclones reach their maximum depths, and the mean distance is 300 km between the surface and the 500-hPa level cyclone centers when the surface cyclones obtain their maturity. According to the authors’ definition of vertical organization, explosively developing cyclones are vertically very well organized systems, whose surface development is antecedent to their 500-hPa level counterpart. Over 1979–2001 cyclones have increased in their system density, intensity, and translational velocity but decreased in their scale at almost all levels. However, some of the trends are not statistically significant. The proportion of vertically well organized systems in the entire population of SH winter extratropical cyclones has considerably increased over the last 23 yr, and the mean distance between the surface and the 500-hPa- level cyclone centers has decreased. Such changes in vertical organization of extratropical cyclones are statistically significant at the 95% confidence level.
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Dissertations / Theses on the topic "Cyclones"

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Petty, Kevin R. "The effects of synoptic factors on the intensities of tropical cyclones over the eastern North Pacific Ocean." The Ohio State University, 1997. http://catalog.hathitrust.org/api/volumes/oclc/39803779.html.

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Spollen, Rachael A. "Meteorological and model traits knowledge bases for North Indian Ocean tropical cyclones." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2002. http://library.nps.navy.mil/uhtbin/hyperion-image/02sep%5FSpollen.pdf.

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Thesis (M.S. in Meteorology and Physical Oceanography)--Naval Postgraduate School, September 2002.
Thesis advisor(s): Russell L. Elsberry, Patrick A. Harr, Mark A. Boothe. Includes bibliographical references (p. 119-120). Also available online.
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Fu, Bing. "An observational analysis of tropical cyclogenesis in the Western North Pacific." Thesis, University of Hawaii at Manoa, 2003. http://hdl.handle.net/10125/7030.

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Budzko, David C. "North Pacific tropical cyclones and teleconnections." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://handle.dtic.mil/100.2/ADA432435.

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Ford, Debra M. "Forecasting tropical cyclone recurvature using an empirical othogonal [sic] function representation of vorticity fields." Thesis, Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA238489.

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Thesis (M.S. in Meteorology and Oceanography)--Naval Postgraduate School, September 1990.
Thesis Advisor(s): Elsberry, Russell L. ; Harr, Patrick A. "September 1990." Description based on title screen as viewed on December 16, 2009. DTIC Identifier(s): EOF (empirical orthogonal functions). Author(s) subject terms: Tropical cyclones, recurvature, empirical orthogonal functions. Includes bibliographical references (p. 73-74). Also available in print.
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Miller, Ronald J. "An Investigation of the ERICA IOP-2 Cyclone Using the NORAPS Model." Thesis, Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA237683.

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Thesis (M.S. in Meteorology)--Naval Postgraduate School, June 1990.
Thesis Advisor(s): Wash, Carlyle H. Second Reader: Nuss, Wendell L. "June 1990." Description based on title screen as viewed on October 19, 2009. DTIC Indicator(s): Weather forecasting, computerized simulation, cyclogenesis, ERICA (Experiment on Rapidly Intensifying Cycloner over the Atlantic), NORAPS (Naval Operational Regional Atmospheric Prediction System), Theses. Author(s) subject terms: Rapid cyclogenesis, ERICA, NORAPS. Includes bibliographical references (p. 77-79). Also available in print.
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Dorics, Theodore G. "An assessment of NOGAPS performance in the prediction of tropical Atlantic circulation formation." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2002. http://library.nps.navy.mil/uhtbin/hyperion-image/02Jun%5FDorics.pdf.

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Patterson, Peter A. "High temperature cyclones." Thesis, McGill University, 1989. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=75974.

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Gas-solids separation was studied in a 102 mm diameter conventional cyclone operated with air heated to temperatures between 300 K and 2 000 K. Cyclone pressure drops, fractional and overall collection efficiencies were measured as functions of temperature, gas throughput, dust loading and cyclone geometry. Alumina and silica of 100% less than 44 $ mu$m mass median diameter were used as test dusts. Inlet velocities ranged from 3 to 42 m/s and inlet dust loadings were between 0.3 and 235 g/m$ sp3$.
Empirical models were derived to correlate the experimental results for the cyclone collection efficiency, pressure drop, tangential velocity and 50% cut size. The performance of the cyclones at very high temperatures was not significantly different from the room temperature behavior, provided that the effect of temperature on particle, gas and flow properties was adequately treated.
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Du, Jun 1962. "Short-range ensemble forecasting of an explosive cyclogenesis with a limited area model." Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/191197.

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Since the atmosphere is a chaotic system, small errors in the initial condition of any numerical weather prediction (NWP) model amplify as the forecast evolves. To estimate and possibly reduce the uncertainty of NWP associated with initial-condition uncertainty (ICU), ensemble forecasting has been proposed which is a method of, differently from the traditional deterministic forecasting, running several model forecasts starting from slightly different initial states. In this dissertation, the impact of ICU and short-range ensemble forecasting (SREF) on quantitative precipitation forecasts (QPFs), as well as on sea-level cyclone position and central pressure, is examined for a case of explosive cyclogenesis that occurred over the contiguous United States. A limited-area model (the PSU/NCAR MM4) is run at 80-km horizontal resolution and 15 layers to produce a 25-member, 36-h forecast ensemble. Lateral boundary conditions for the MM4 model are provided by ensemble forecasts from a global spectral model (the NCAR CCM1). The initial perturbations of the ensemble members possess a magnitude and spatial decomposition which closely match estimates of global analysis error, but they were not dynamically-conditioned. Results for 80-km ensemble forecast are compared to forecasts from the then operational Nested Grid Model (NGM), a single 40-km MM4 forecast, and a second 25-member MM4 ensemble based on a different cumulus parameterization and slightly different initial conditions. Acute sensitivity to ICU marks ensemble QPF and the forecasts of cyclone position and central pressure. Ensemble averaging always reduces the rms error for QPF. Nearly 90% of the improvement is obtainable using ensemble sizes as small as 8-10. However, ensemble averaging can adversely affect the forecasts related to precipitation areal coverage because of its smoothing nature. Probabilistic forecasts for five mutually exclusive, completely exhaustive categories are found to be skillful relative to a climatological forecast. Ensemble sizes of --, 10 can account for 90% of improvement in probability density function. Our results indicate that SREF techniques can now provide useful QPF guidance and increase the accuracy of precipitation, cyclone position, and cyclone's central pressure forecasts. With current analysis/forecast systems, the benefit from simple ensemble averaging is comparable to or exceed that obtainable from improvement in the analysis/forecast system.
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Wang, Lei. "Study of tropical cyclogenesis over the South China Sea /." View abstract or full-text, 2008. http://library.ust.hk/cgi/db/thesis.pl?MATH%202008%20WANG.

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Books on the topic "Cyclones"

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Newton, Chester W., and Eero O. Holopainen, eds. Extratropical Cyclones. Boston, MA: American Meteorological Society, 1990. http://dx.doi.org/10.1007/978-1-944970-33-8.

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LeBorgne, Jean. Les cyclones. Paris: Presses Universitaires de France, 1986.

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Close, Edward. Cyclones, tornades ... Montréal, Québec: Petit homme, Une société de Québecor Média, 2013.

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Borgne, Jean Le. Les Cyclones. Paris: Presses Universitaires de France, 1986.

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Borgne, Jean Le. Les cyclones. Paris: Presses universitaires de France, 1986.

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Blake, Eric S. Tropical cyclones of the eastern North Pacific Basin, 1949-2006. Ashville, North Carolina: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service-National Environmental Satellite, Data, and Information Service, 2009.

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Blake, Eric S. Tropical cyclones of the eastern North Pacific Basin, 1949-2006. Ashville, North Carolina: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service-National Environmental Satellite, Data, and Information Service, 2009.

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Das, Manoj. Cyclones: A novel. New Delhi: Sterling Publishers, 1987.

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Das, Manoj. Cyclones: A novel. London: Oriental University Press, 1987.

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K, Hall Michelle, ed. Exploring tropical cyclones. Belmont, CA: Thomson Brooks/Cole, 2007.

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Book chapters on the topic "Cyclones"

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Leith, David, and Donna Lee Jones. "Cyclones." In Handbook of Powder Science & Technology, 727–52. Boston, MA: Springer US, 1997. http://dx.doi.org/10.1007/978-1-4615-6373-0_15.

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Coury, José Renato, Reinaldo Pisani, and Yung-Tse Hung. "Cyclones." In Air Pollution Control Engineering, 97–151. Totowa, NJ: Humana Press, 2004. http://dx.doi.org/10.1007/978-1-59259-778-9_3.

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Bourdé, Arnaud, Xavier Combes, and Patrick Portecop. "Cyclones." In Disaster Medicine Pocket Guide: 50 Essential Questions, 81–84. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-00654-8_17.

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Ginis, Isaac. "Tropical Cyclones." In From Hurricanes to Epidemics, 121–28. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-55012-7_10.

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Hoffmann, Alex C., and Louis E. Stein. "Demisting Cyclones." In Gas Cyclones and Swirl Tubes, 239–62. Berlin, Heidelberg: Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-07377-3_13.

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Camargo, Suzana J., and Solomon M. Hsiang. "Tropical Cyclones." In Extreme Events, 303–42. Hoboken, NJ: John Wiley & Sons, Inc, 2015. http://dx.doi.org/10.1002/9781119157052.ch18.

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Reilly, Benjamin. "Tropical Cyclones." In Disasters in World History, 211–47. New York: Routledge, 2024. http://dx.doi.org/10.4324/9781003436805-7.

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Lackmann, Gary. "Extratropical Cyclones." In Midlatitude Synoptic Meteorology, 95–129. Boston, MA: American Meteorological Society, 2011. http://dx.doi.org/10.1007/978-1-878220-56-1_5.

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Williams, Jack. "Tropical Cyclones." In The AMS Weather Book: The Ultimate Guide to America’s Weather, 228–57. Boston, MA: American Meteorological Society, 2009. http://dx.doi.org/10.1007/978-1-935704-55-3_10.

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Perevalova, Natalia. "Tropical Cyclones." In Exploring Natural Hazards, 49–74. Boca Raton, FL : CRC Press, 2018.: Chapman and Hall/CRC, 2018. http://dx.doi.org/10.1201/9781315166858-2.

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Conference papers on the topic "Cyclones"

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Ni, Weicheng, Ad Stoffelen, Kaijun Ren, Jur Vogelzang, Yanlai Zhao, and Wuxin Wang. "Monitoring of Tropical Cyclones at Enhanced Resolution." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium, 5803–6. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10642968.

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Pascual, Daniel, Christopher Ruf, and Rajeswari Balasubramaniam. "Azimuthal Dependence of CYGNSS Winds in Tropical Cyclones." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium, 5835–38. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10640920.

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May, Joshua, Mehrtash Harandi, J. Scott Tyo, Liang Hu, and Elizabeth A. Ritchie-Tyo. "A CNN system for segmenting tropical cyclones neighborhoods in geostationary images." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium, 8259–62. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10641684.

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Tao, Shanshan, Jialing Song, Zhifeng Wang, Yong Liu, and Sheng Dong. "Statistical Analysis for the Duration and Time Intervals of Tropical Cyclones, Hong Kong." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95791.

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Abstract Hong Kong is impacted by tropical cyclones from April to December each year. The duration of tropical cyclones is one key factor to impact the normal operation of port or coastal engineering, and longer time interval between two tropical cyclones can provide longer operation or construction time. Therefore, it is quite important to study on the long-term laws of the duration and time intervals of tropical cyclones which attacked Hong Kong. The Hong Kong Observatory issues the warning signals to warn the public of the threat of winds associated with a tropical cyclone. Choose the tropical cyclones with warning signal No. 3 or above as the research object. A statistical study was conducted on the duration of each tropical cyclone, the time interval between every two continuous tropical cyclones during the year, and the time interval between the last cyclone of each year and the first cyclone of the following year. Poisson compound extreme value distributions are constructed to calculate the return values, which can make people know how long a tropical cyclone with a fixed duration or time interval occurs once in statistical average sense. Based on bivariate copulas, the joint probability distribution of duration and time intervals of tropical cyclones are presented. Then when the duration of a tropical cyclone is known, the conditional probability that the time interval before the next tropical cyclone occurs is greater than a certain value can be calculated. The results provide corresponding conditional probability distributions. Similarly, for the sum of the duration of tropical cyclones each year, and the time interval between the last cyclone of each year and the first cyclone of the following year, their joint probability distribution and conditional probability distributions are also presented. The conditional probability can provide the probabilistic prediction of the length of the stationary period (with no impact of tropical cyclones).
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Gramcianinov, C. B., R. M. Campos, C. Guedes Soares, and R. de Camargo. "Comparison Between ERA5 and CFS Datasets of Extratropical Cyclones Associated With Extreme Wave Events in the Atlantic Ocean." In ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-18488.

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Abstract Atmospheric and ocean datasets using numerical modeling allied to data assimilation are valuable tools for planning and maintaining marine activities, particularly due to their spatial coverage and resolution. However, even modern analyses and reanalyses present critical errors where cyclonic winds are often underestimated in some locations, leading to issues in wind-wave climate hindcasts and forecasts. This work aims to evaluate two of the newest datasets available regarding their ability to reproduce extratropical cyclone tracks associated with extreme waves in the Atlantic Ocean. The analysis is focused on the storm track position and cyclone intensity, two important features that control the wave climate. The datasets used are the ECMWF’s ERA5 and NCEP’s CFSv2. The cyclones are identified and compared between 2011 and 2018 using the relative vorticity at 850hPa and the intensity is measured through the 10-meters wind speed. The results show that the differences in track density exist mainly in coastal areas and they can be related to the coarser resolution of CFSv2 compared to ERA5. CFSv2 presents a higher number of cyclones associated with extreme wave events in the South and North Atlantic, corresponding to 87.1% and 89.2% of the cyclones identified, while ERA5 presents 66.6% and 59.5% respectively. The maximum intensity distribution shows that CFSv2 tends to produce more intense cyclones than ERA5, even for identical storms in the datasets. The distances of matching cyclones in the two datasets are around 0.5°.
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Whelan, J. R., Y. Drobyshevski, and J. D. McConochie. "Frequency and Time Domain Analyses of Vessel Motions During Tropical Cyclones." In ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-80098.

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A permanently turret moored floating facility located off the North West coast of Australia is likely to be exposed to tropical cyclones, which exhibit extreme wave height, wind and surface currents. Furthermore the cyclonic eye and fringes are characterised by rapidly varying metocean conditions, particularly wind speed and direction. It is necessary to understand the weather vaning and motion responses of the vessel during these transient conditions for successful facility development. This paper presents weather vaning and motion analyses of a Floating Storage and Offloading (FSO) vessel during the passage of tropical cyclones. A synthetic tropical data base developed by Woodside Energy Limited was used to generate the cyclonic conditions. The data base contains storms with return periods ranging from 10 to 100,000 years. Time histories of wave spectrum, wind and current at half-hourly intervals for several cyclones were examined. The weather vaning and motions responses of the FSO were computed using two methods: (1) a frequency domain quasi-stationary approach, and (2) a time domain approach. In the frequency domain analyses the metocean conditions were treated as stationary for each half-hour interval and the mean vessel heading and most probable amplitudes of motions were calculated. In the time domain analyses, the time histories of metocean conditions were closely matched to the synthesised cyclonic conditions, and time histories of vessel heading and motion responses were generated. Multiple realisations were simulated for each cyclone to assess variability of results associated with wave train random seed. A key finding of the study is that the worst roll response tends to occur after the eye of the cyclone has passed, at which time the wind and waves were highly non-collinear. At this time the vessel weather vanes so as to experience waves which are substantially beam-on. When the cyclonic eye is directly over the site, there is a reduction in wind speed and as a consequence the vessel weather vanes into the sea. This causes a corresponding reduction in the roll response. Results from both analysis methods have been compared and good agreement is observed. The applicability and limitations of the two analyses methods are also considered.
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Bhavithra, R. S., and S. A. Sannasiraj. "Cyclonic Wave Field in the Bay of Bengal Region Under Changing Climate Scenarios." In ASME 2022 41st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2022. http://dx.doi.org/10.1115/omae2022-79092.

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Abstract Wind-wave plays a major role in the planning and designing of important coastal structures. The study on wave characteristics is considered necessary for the routing of ships, wave hindcasting and forecasting. Climate change is one of the major threat that has been occurring over the years and the impact of climate change on wave climate results in increased storm effects and rough sea conditions. Bay of Bengal (BOB), an active cyclonic region along the North Indian Ocean experiences severe storms every year during the north-east monsoon season. Hence, an understanding of wind-wave climate under cyclonic storms in the BOB region is essential. The present study considers three severe cyclonic storms in the BOB region: Phailin which occurred during October 2013; Hudhud during October 2014; and, Vardah during December 2016. The study further details about the impact caused by these cyclone when projected to the future under the climate change scenarios. The wave climate of the three considered cyclones is projected for the Representative Concentration Pathway (RCP) scenarios of RCP4.5, RCP6.0 and RCP8.5 under both for the Near-Future (2035) and Far-Future (2075) categories. The domain covering the BOB region is discretized with a resolution of 0.25°x0.25°. The surface wind of the chosen domain for the projected scenarios is obtained from the Weather Research and Forecasting (WRF) model and then these winds are forced into the WAve Model (WAM) to predict the corresponding wave climate. The significant wave height (Hs) obtained from the WAM model for the projected scenarios has been compared to the present scenario of the respective cyclones and the results show an increase in intensity for all the three cyclones under the Far-Future categories of RCP6.0 and RCP8.5 scenarios. The wave climate under Hudhud cyclone has the greatest intensity of about 21% under the Far-Future category.
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Grey, Stephen, and Ye Liu. "A Probabilistic Approach to Tropical Cyclone Modelling." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-96245.

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Abstract Tropical cyclones are highly variable and, in many areas of the world, are the main cause of extreme wind and associated waves, surge and current conditions. At a given location, cyclones that cause a significant impact are relatively rare but severe events, which means that the number of historical events for which data are available is often quite small. In addition, the effects, particularly surge, can be relatively localized and affected by the local bathymetry and topography. This causes considerable difficulty in making quantitative predictions of extreme events for design of offshore or coastal structures in areas affected by tropical cyclones. A new probabilistic method has been developed to increase the sample of tropical cyclones by producing 10,000 years of synthetic cyclone tracks with a range of paths, intensities and sizes based on Hall and Jewson [1] and Casson and Coles [2]. From this set of synthetic tracks, those tropical cyclones most likely to affect the site of interest are modelled using time-varying wind fields based on the Holland model [3] with surge, current and waves then modelled using the hydrodynamic model TELEMAC-2D coupled to the SWAN wave model. As it is impractical to model 10,000 years of tropical cyclones, a Gaussian process emulator is employed to relate the resultant conditions to parameters defining the cyclones, such as track position, heading, intensity and radius to maximum wind. The result is a synthesized 10,000 years of cyclone events from which design conditions for a range of return periods can be predicted with a greater degree of certainty than by extrapolating from historical events.
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Lalak, Ireneusz, Joachim Seeber, Frank Kluger, and Stanislaw Krupka. "Operational Experience With High Efficiency Cyclones: Comparison Between Boiler A and B in the Zeran Power Plant — Warsaw, Poland." In 17th International Conference on Fluidized Bed Combustion. ASMEDC, 2003. http://dx.doi.org/10.1115/fbc2003-146.

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The two 450t/h CFB units of the Zeran heat and power plant in Warsaw, Poland, are nearly identical in design, except for the cyclones. While the first CFB unit Zeran A which was commissioned in 1995 had cyclones of a prior design, the second unit Zeran B, which went into operation in late 2001, was equipped with high efficiency cyclones with the latest technological developments. The impact of the cyclone design is clearly visible in the operational data. Due to the high cyclone efficiency, the internal circulation became much higher and the fineness of the circulating particles was shifted to finer particles. As a result, the heat transfer in the furnace was boosted and the temperature profile became more even. This had a significant positive effect on the emissions, especially NOx and on the limestone consumption, which was considerably reduced.
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Gramcianinov, C. B., R. M. Campos, R. de Camargo, and C. Guedes Soares. "Relation Between Cyclone Evolution and Fetch Associated With Extreme Wave Events in the South Atlantic Ocean." In ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-18486.

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Abstract Extreme wave generation in middle and high latitudes is mainly associated with extratropical cyclones. The wave generation process depends on the size and orientation of the fetch associated with each cyclone, which is usually not taken into account in traditional statistical approaches. A better understanding of the combined effect of the fetch orientation, displacement, and position within the extratropical cyclone can contribute with more accurate wave hindcasts and forecasts, which are crucial to marine operations. The main goal of this work is to investigate the fetch patterns and configurations associated with extratropical cyclones that promote extreme wave events in the western portion of the South Atlantic Ocean. Cyclones are tracked using an objective algorithm and linked to winter extreme Hs events in 10 years of ERA5. The results show the occurrence of 11.4 ± 2.8 storms per winter associated with extreme waves within the domain. Among these extreme events, the maximum and mean Hs was 10.3m and 6.1m respectively. The analysis of the fetch evolution during the lifecycle of the cyclones associated with the 10 most extreme events showed that the surface winds present its maximum usually 12h to 24h before the maximum Hs. The spatial pattern of the most severe events shows the development of a large fetch along the continental shelf, usually within the cold sector of the cyclone.
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Reports on the topic "Cyclones"

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Noy, Ilan, Miloud Lacheheb, and Madhavi Pundit. The Impact of Tropical Cyclones on Fishing Activities in the Philippines. Asian Development Bank, August 2023. http://dx.doi.org/10.22617/wps230291-2.

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This study looks at fishing activity in the Philippines’ Exclusive Economic Zone in 2012, as well as how it responded to tropical cyclones. The study identifies the main fishing grounds and examines the impact of tropical cyclone speed on vessel position using satellite images and tropical cyclones data. Data suggest that tropical cyclones have a negative impact on fishing activity, with fewer active boats during and after the storm. The most affected locations include the Sibuyan Sea, Visayan Sea, and Panay Gulf. These tropical cyclones were estimated to reduce commercial fishing production by 7,800 tons per day, affecting more than 188,000 families in Western Visayas.
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Naguib, Costanza, Martino Pelli, David Poirier, and Jeanne Tschopp. The Impact of Cyclones on Local Economic Growth: Evidence from Local Projections. CIRANO, August 2022. http://dx.doi.org/10.54932/xvof3031.

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We shed new light on the short-term dynamic effects of cyclones on local economic growth in India. We proxy local GDP growth with night-time light intensity data and construct a cyclone index that varies across months and districts depending on windspeed exposures. Using local projections on highly granular data for the period 1993M1-2011M12, we find that yearly estimations hide large short-term differential impacts and that the negative impact of cyclones is the largest between 4 and 8 months after the event.
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Holland, Greg J., Yuqing Wang, Peter May, Jeff Kepert, and Lance Leslie. Mesoscale Processes In Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada610207.

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Smith, Roger K. The Dynamics of Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada629427.

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Smith, Roger K. The Dynamics of Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 2003. http://dx.doi.org/10.21236/ada629939.

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Smith, Roger K. The Dynamics of Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630961.

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Holland, Greg J., Yuqing Wang, Peter May, Jeff Kepert, and Lance Leslie. Mesoscale Processes in Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630971.

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Leslie, Lance. Mesoscale Processes in Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada624227.

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Smith, Roger K. The Dynamics of Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada624625.

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Smith, Roger K. The Dynamics of Tropical Cyclones. Fort Belvoir, VA: Defense Technical Information Center, August 2001. http://dx.doi.org/10.21236/ada625686.

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