Does It Make Sense to Modify Tropical Cyclones? a Decision-Analytic Assessment
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Bonnie 19-30 August 1998
PRELIMINARY REPORT Hurricane Bonnie 19-30 August 1998 Lixion A. Avila National Hurricane Center 24 October 1998 Bonnie was the third hurricane to directly hit the coast of North Carolina during the past three years. a. Synoptic History The origin of Bonnie was a large and vigorous tropical wave that moved over Dakar, Senegal on 14 August. The wave was depicted on visible satellite imagery by a large cyclonic low- to mid-level circulation void of deep convection. The wave caused a 24-h surface pressure change of -3.5 and -4.0 mb at Dakar and Sal respectively. There was a well established 700 mb easterly jet which peaked at 50 knots just before the wave axis crossed Dakar, followed by a well marked wind-shift from the surface to the middle troposphere. The overall circulation exited Africa basically just north of Dakar where the ocean was relatively cool. However, a strong high pressure ridge steered the whole system on a west- southwest track over increasingly warmer waters and convection began to develop. Initially, there were several centers of rotation within a much larger circulation and it was not until 1200 UTC 19 August that the system began to consolidate and a tropical depression formed. Although the central area of the tropical depression was poorly organized, the winds to the north of the circulation were nearing tropical storm strength. This was indicated by ship observations and high resolution low-cloud wind vectors provided in real time by the University of Wisconsin. T h e depression was then upgraded to Tropical Storm Bonnie based on these winds and satellite intensity estimates at 1200 UTC 20 August. -
Hurricane.Pdf
AUGUST 2009 N O T E S A N D C O R R E S P O N D E N C E 2481 NOTES AND CORRESPONDENCE Inertial Particle Dynamics in a Hurricane THEMISTOKLIS SAPSIS AND GEORGE HALLER Massachusetts Institute of Technology, Cambridge, Massachusetts (Manuscript received 23 June 2008, in final form 8 February 2009) ABSTRACT The motion of inertial (i.e., finite-size) particles is analyzed in a three-dimensional unsteady simulation of Hurricane Isabel. As established recently, the long-term dynamics of inertial particles in a fluid is governed by a reduced-order inertial equation, obtained as a small perturbation of passive fluid advection on a globally attracting slow manifold in the phase space of particle motions. Use of the inertial equation enables the visualization of three-dimensional inertial Lagrangian coherent structures (ILCS) on the slow manifold. These ILCS govern the asymptotic behavior of finite-size particles within a hurricane. A comparison of the attracting ILCS with conventional Eulerian fields reveals the Lagrangian footprint of the hurricane eyewall and of a large rainband. By contrast, repelling ILCS within the eye region admit a more complex geometry that cannot be compared directly with Eulerian features. 1. Introduction a. Prior work on coherent structures in hurricanes Our focus here is the dynamics of inertial (i.e., small Although the prediction of hurricane tracks has consid- but finite) particles in the three-dimensional flow field of erably improved over the past decades, there is still sub- Hurricane Isabel (cf. Fig. 1). Inertial particles in a fluid stantial room for improvement in hurricane intensity are typically modeled as small spherical objects whose forecasting (Houze et al. -
Atlantic Hurricane Season of 1998
DECEMBER 2001 ANNUAL SUMMARY 3085 Atlantic Hurricane Season of 1998 RICHARD J. PASCH,LIXION A. AVILA, AND JOHN L. GUINEY National Hurricane Center, Tropical Prediction Center, NOAA/NWS, Miami, Florida (Manuscript received 30 June 2000, in ®nal form 18 June 2001) ABSTRACT The 1998 hurricane season in the Atlantic basin is summarized, and the individual tropical storms and hurricanes are described. It was an active season with a large number of landfalls. There was a near-record number of tropical cyclone±related deaths, due almost entirely to Hurricane Mitch in Central America. Brief summaries of forecast veri®cation and tropical wave activity during 1998 are also presented. 1. Introduction case in 1995 and 1996, most of the TCs originated in the deep Tropics south of latitude 208N. Nineteen ninety-eight was an active year for tropical Figure 2 shows the sea surface temperature anomalies cyclones (TCs) in the Atlantic basin. Fourteen tropical from the long-term mean for August through October storms developed; 10 of these tropical storms became of 1998. Practically all of the 1998 TCs occurred during hurricanes. The long-term average numbers of tropical storms and hurricanes per season are 10 and 6, respec- these months. During this period nearly all of the At- tively. From 1995 through 1998, 33 hurricanes occurred, lantic Ocean's surface from the equator to 608N was the largest 4-yr total ever observed (going back to at warmer than normal. Of particular interest is the tropical least the start of reliable records in the mid-1940s). region from the Caribbean Sea eastward to near the coast Three of the 1998 hurricanes strengthened into major of Africa. -
Numerical Simulation of Hurricane Bonnie (1998). Part I: Eyewall Evolution and Intensity Changes
JANUARY 2004 ZHU ET AL. 225 Numerical Simulation of Hurricane Bonnie (1998). Part I: Eyewall Evolution and Intensity Changes TONG ZHU AND DA-LIN ZHANG Department of Meteorology, University of Maryland, College Park, College Park, Maryland FUZHONG WENG NOAA/NESDIS Of®ce of Research and Applications, Camp Springs, Maryland (Manuscript received 13 November 2002, in ®nal form 18 July 2003) ABSTRACT In this study, a 5-day explicit simulation of Hurricane Bonnie (1998) is performed using the ®fth-generation Pennsylvania State University±National Center for Atmospheric Research Mesoscale Model (MM5) with the ®nest grid length of 4 km. The initial mass, wind, and moisture ®elds of the hurricane vortex are retrieved from the Advanced Microwave Sounding Unit-A (AMSU-A) satellite measurements, and the sea surface temperature (SST) is updated daily. It is shown that the simulated track is within 38 latitude±longitude of the best track at the end of the 5-day integration, but with the landfalling point close to the observed. The model also reproduces reasonably well the hurricane intensity and intensity changes, asymmetries in cloud and precipitation, as well as the vertical structures of dynamic and thermodynamic ®elds in the eye and eyewall. It is shown that the storm deepens markedly in the ®rst 2 days, during which period its environmental vertical shear increases substantially. It is found that this deepening could occur because of the dominant energy supply by a strong low-level southeasterly ¯ow into the eastern eyewall plus the presence of underlying warm SST and favorable upper-level divergent out¯ow. However, the approaching of a strong upper-level northwesterly ¯ow tends to generate mass convergence and subsidence warming and drying, thereby suppressing the devel- opment of deep convection in the western semicircle. -
Numerical Simulation of Hurricane Bonnie (1998)
JANUARY 2004 ZHU ET AL. 225 Numerical Simulation of Hurricane Bonnie (1998). Part I: Eyewall Evolution and Intensity Changes TONG ZHU AND DA-LIN ZHANG Department of Meteorology, University of Maryland, College Park, College Park, Maryland FUZHONG WENG NOAA/NESDIS Of®ce of Research and Applications, Camp Springs, Maryland (Manuscript received 13 November 2002, in ®nal form 18 July 2003) ABSTRACT In this study, a 5-day explicit simulation of Hurricane Bonnie (1998) is performed using the ®fth-generation Pennsylvania State University±National Center for Atmospheric Research Mesoscale Model (MM5) with the ®nest grid length of 4 km. The initial mass, wind, and moisture ®elds of the hurricane vortex are retrieved from the Advanced Microwave Sounding Unit-A (AMSU-A) satellite measurements, and the sea surface temperature (SST) is updated daily. It is shown that the simulated track is within 38 latitude±longitude of the best track at the end of the 5-day integration, but with the landfalling point close to the observed. The model also reproduces reasonably well the hurricane intensity and intensity changes, asymmetries in cloud and precipitation, as well as the vertical structures of dynamic and thermodynamic ®elds in the eye and eyewall. It is shown that the storm deepens markedly in the ®rst 2 days, during which period its environmental vertical shear increases substantially. It is found that this deepening could occur because of the dominant energy supply by a strong low-level southeasterly ¯ow into the eastern eyewall plus the presence of underlying warm SST and favorable upper-level divergent out¯ow. However, the approaching of a strong upper-level northwesterly ¯ow tends to generate mass convergence and subsidence warming and drying, thereby suppressing the devel- opment of deep convection in the western semicircle. -
A Chronology of Notable Weather Events by Douglas V. Hoyt
A Chronology of Notable Weather Events by Douglas V. Hoyt Edition of 8/4/2011 243 A. D. An inundation of the sea in Lincolnshire laid under water many thousands of acres (Camden). 353 Flood in Cheshire in which 3000 people died along with thousands of cattle (Hayden). 402 Euxine Sea frozen over for 20 days (Hayden) 500 The Vandals from Poland held Western Africa, the Diocese of Africa, Visigoth (Western Goth) from Scandia held Spain, Ostrogoth (Eastern Goth) from Scandia held Italy, Germanic-Franks from Scandia held Gaul, Burgundians held Rhone river, and Celts, Germanic-Anglo-Saxon held the diocese of England. The massive migration of the Mongols, the Huns, Goth, Slav-Bulgars, and Avars westward is because of adverse weather conditions driving them from their lands . The Germanic-Danes inhabited the Danish Islands, Schonen, and later Jutland. St. Brendan (521-527) in his voyage to the northwest suggests the Celts of Ireland discovered America about this time. The Polynesian reached Hawaii and established agricultural settlements. These people had traveled 2500 miles from Island to Island. It is inconceivable that these peoples didn't reach America in the past 500 years. The Polynesians colonized Hawaii, Easter Island, and Madagascar by 500 A.D. 507 Men from Tsinngan, China report being blown across the Great Sea East to a people who speak a strange language. 508 In England, the rivers were frozen for more than two months (including Thames?). Possible severe winter. Rivers frozen for two months. Years also quoted as 507 or 509. 514 St. Brendan (484-577) of Ireland explored the area discovering the Hebrides, Orkney, Faeroe Islands and Iceland, starting about this time. -
Quantifying Hurricane Wind Speed with Undersea Sound
Quantifying Hurricane Wind Speed with Undersea Sound by Joshua David Wilson B.S., Mechanical Engineering, University of Idaho (1999) Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY and the WOODS HOLE OCEANOGRAPHIC INSTITUTION June 2006 @ Joshua David Wilson, MMVI. All rights reserved. The author hereby grants to MIT and WHO1 permission to reproduce and distribute publicly paper and electronic copies of this thesis document in whole or in part. Author Massachusetts Institute of Technology and Woods Hole Oceanographic Institution June, 2006 Certified by. ..... Nicholas C. Makris rofessor of Mechanical Engineering Thesis Supervisor Accepted by ......... ...................................... Henrik Schmidt for Applied Ocean Science and Engineering y and Woods Hole Oceanographic Institution ............................ Lallit Anand Chair, Commit tee on Graduate Students, Department of Mechanical Engineering Quantifying Hurricane Wind Speed with Undersea Sound Joshua David Wilson Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy June, 2006 Abstract Hurricanes, powerful storms with wind speeds that can exceed 80 m/s, are one of the most destructive natural disasters known to man. While current satellite technology has made it possible to effectively detect and track hurricanes, expensive 'hurricane- hunting' aircraft are required to accurately classify their destructive power. Here we show that passive undersea acoustic techniques may provide a promising tool for accurately quantifying the destructive power of a hurricane and so may provide a safe and inexpensive alternative to aircraft-based techniques. It is well known that the crashing of wind-driven waves generates underwater noise in the 10 Hz to 10 kHz range. -
Tropical Cyclones Affecting North Carolina Since 1586: an Historical
NOAA Technical Memorandum NWS ER-100 TROPICAL CYCLONES AFFECTING NORTH CAROLINA SINCE 1586 - AN HISTORICAL PERSPECTIVE JAMES E. HUDGINS National Weather Service Office Blacksburg, Virginia Scientific Services Division Eastern Region Headquarters Bohemia, New York October 2007 U.S. DEPARTMENT OF National Oceanic and National Weather Service COMMERCE Atmospheric Administration NOAA TECHNICAL MEMORANDA National Weather Service, Eastern Region Subseries The National Weather Service Eastern Region (ER) Subseries provides an informal medium for the documentation and quick dissemination of results not appropriate, or not yet ready for formal publications. The series is used to report on work in progress, to describe technical procedures and practices, or to relate progress to a limited audience. These Technical Memoranda will report on investigations devoted primarily to regional and local problems of interest mainly to ER personnel, and usually will not be widely distributed. Papers 1 to 22 are in the former series, ESSA Technical Memoranda, Eastern Region Technical Memoranda (ERTM); papers 23 to 37 are in the former series, ESSA Technical Memoranda, Weather Bureau Technical Memoranda (WBTM). Beginning with 38, the papers are now part of the series, NOAA Technical Memoranda NWS. Papers 1 to 22 are available from the National Weather Service Eastern Region, Scientific Services Division, 630 Johnson Avenue, Bohemia, NY, 11716. Beginning with 23, the papers are available from the National Technical Information Service, U.S. Department of Commerce, Sills Bldg., 5285 Port Royal Road, Springfield, VA 22161. Prices vary for paper copy and for microfiche. Order by accession number shown in parentheses at end of each entry. ESSA Technical Memoranda ERTM 1 Local Uses of Vorticity Prognoses in Weather Prediction. -
Preliminary Report Hurricane Danielle 24 August - 3 September, 1998
Preliminary Report Hurricane Danielle 24 August - 3 September, 1998 Richard J. Pasch National Hurricane Center 19 January, 1999 Danielle had a long track across the Atlantic. Although it did not seriously impact land as a tropical cyclone, it battered portions of Great Britain as an extratropical system. a. Synoptic History A tropical wave moved off the west coast of Africa on 21 August accompanied by disorganized cloudiness and showers. Within 24 hours, deep convection became somewhat more consolidated in clusters near an ill-defined center of cyclonic cloud rotation. Initial Dvorak technique classifications were assigned at 1100 UTC 22 August. Thereafter, the organization of the disturbance continued to gradually improve as cloudiness and showers became concentrated in a circular area. By 0600 UTC 24 August, the Dvorak T-number was analyzed at 2.0 and it is estimated that Tropical Depression Four formed around this time, centered a little less than 600 n mi west-southwest of the Cape Verde Islands (Fig. 1 and Table 1 give the overall “best track” of this system). Strengthening continued, as satellite images showed convection becoming more tightly wrapped around the center, and the tropical cyclone is estimated to have become Tropical Storm Danielle by 1800 UTC 24 August. Upper-tropospheric outflow was well-defined over the area, and Danielle intensified further. The first visible satellite pictures on 25 August revealed a “pinhole” eye, indicating that the system had become a hurricane. Danielle was a quite compact system, with tropical storm force winds covering an area estimated to be only a little more than 100 n mi in diameter.