2009 HFIP Activities
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The 2009 Atlantic Hurricane Season in Perspective by Dr
AIRCURRENTS THE 2009 ATLANTIC EDITor’s noTE: November 30 marked the official end of the Atlantic HURRICANE SEASON hurricane season. With nine named storms, including three hurricanes, and no U.S. landfalling hurricanes, this season was the second quietest since IN PERSPECTIVE 1995, the year the present period of above-average sea surface temperatures (SSTs) began. This year’s relative inactivity stands in sharp contrast to the 2008 season, during which Hurricanes Dolly, Gustav, and Ike battered the Gulf Coast, causing well over 10 billion USD in insured losses. With no U.S. landfalling hurricanes in 2009, but a near miss in the Northeast, 2009 reminds us yet again of the dramatic short term variability in hurricane 12.2009 landfalls, regardless of whether SSTs are above or below average. By Dr. Peter S. Dailey HOW DOES ACTIVITY IN 2009 COMPARE TO Hurricanes are much more intense than tropical storms, LONG-TERM AVERAGES? producing winds of at least 74 mph. Only about half of By all standard measures, the 2009 Atlantic hurricane tropical storms reach hurricane strength in a typical year, season was below average. Figure 1 shows the evolution with an average of six hurricanes by year end. Major of a “typical” season, which reflects the long-term hurricanes, with winds of 111 mph or more, are even rarer, climatological average over many decades of activity. with only about three expected in the typical year. Note the Tropical storms, which produce winds of at least 39 mph, sharp increase in activity during the core of the season—the occur rather frequently. -
The Influences of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons
Meteorology Senior Theses Undergraduate Theses and Capstone Projects 2018 The nflueI nces of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons Hannah Messier Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/mteor_stheses Part of the Meteorology Commons Recommended Citation Messier, Hannah, "The nflueI nces of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons" (2018). Meteorology Senior Theses. 40. https://lib.dr.iastate.edu/mteor_stheses/40 This Dissertation/Thesis is brought to you for free and open access by the Undergraduate Theses and Capstone Projects at Iowa State University Digital Repository. It has been accepted for inclusion in Meteorology Senior Theses by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. The Influences of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons Hannah Messier Department of Geological and Atmospheric Sciences, Iowa State University, Ames, Iowa Alex Gonzalez — Mentor Department of Geological and Atmospheric Sciences, Iowa State University, Ames Iowa Joshua J. Alland — Mentor Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, Albany, New York ABSTRACT The summertime behavior of the North Atlantic Subtropical High (NASH), African Easterly Jet (AEJ), and the Saharan Air Layer (SAL) can provide clues about key physical aspects of a particular hurricane season. More accurate tropical weather forecasts are imperative to those living in coastal areas around the United States to prevent loss of life and property. -
ABSTRACT Title of Document: the EFFECT of HURRICANE SANDY
ABSTRACT Title of Document: THE EFFECT OF HURRICANE SANDY ON NEW JERSEY ATLANTIC COASTAL MARSHES EVALUATED WITH SATELLITE IMAGERY Diana Marie Roman, Master of Science, August 2015 Directed By: Professor, Michael S. Kearney, Environmental Science and Technology Hurricane Sandy, one of several large extratropical hurricanes to impact New Jersey since 1900, produced some of the most extensive coastal destruction within the last fifty years. Though the damage to barrier islands from Sandy was well-documented, the effect of Sandy on the New Jersey coastal marshes has not. The objective of this analysis, based on twenty-three Landsat Thematic Mapper (TM) data sets collected between 1984 and 2011 and Landsat 8 Operational Land Imager (OLI) images collected between 2013 and 2014 was to determine the effect of Hurricane Sandy on the New Jersey Atlantic coastal marshes. Image processing was performed using ENVI image analysis software with the NDX model (Rogers and Kearney, 2004). Results support the conclusion that the marshes were stable between 1984 and 2006, but had decreased in vegetation density coverage since 2007. Hurricane Sandy caused the greatest damage to low-lying marshes located close to where landfall occurred. THE EFFECT OF HURRICANE SANDY ON NEW JERSEY ATLANTIC COASTAL MARSHES EVALUATED WITH SATELLITE IMAGERY by Diana Marie Roman Thesis submitted to the Faculty of the Graduate School of the University of Maryland, College Park in partial fulfillment of the requirements for the degree of Masters of Science 2015 Advisory Committee: Professor Michael Kearney, Chair Professor Andrew Baldwin Associate Professor Andrew Elmore © Copyright by Diana Marie Roman 2015 Forward Hurricane storm impacts on coastal salt marshes have increased over time. -
Doppler Radar Analysis of Typhoon Otto (1998) —Characteristics of Eyewall and Rainbands with and Without the Influence of Taiw
Journal of the Meteorological Society of Japan, Vol. 83, No. 6, pp. 1001--1023, 2005 1001 Doppler Radar Analysis of Typhoon Otto (1998) —Characteristics of Eyewall and Rainbands with and without the Influence of Taiwan Orography Tai-Hwa HOR, Chih-Hsien WEI, Mou-Hsiang CHANG Department of Applied Physics, Chung Cheng Institute of Technology, National Defense University, Taiwan, Republic of China and Che-Sheng CHENG Chinese Air Force Weather Wing, Taiwan, Republic of China (Manuscript received 27 October 2004, in final form 26 August 2005) Abstract By using the observational data collected by the C-band Doppler radar which was located at the Green Island off the southeast coast of Taiwan, as well as the offshore island airport and ground weather stations, this article focuses on the mesoscale analysis of inner and outer rainband features of Typhoon Otto (1998), before and after affected by the Central Mountain Range (CMR) which exceeds 3000 m in elevation while the storm was approaching Taiwan in the northwestward movement. While the typhoon was over the open ocean and moved north-northwestward in speed of 15 km/h, its eyewall was not well organized. The rainbands, separated from the inner core region and located at the first and second quadrants relative to the moving direction of typhoon, were embedded with active con- vections. The vertical cross sections along the radial showed that the outer rainbands tilted outward and were more intense than the inner ones. As the typhoon system gradually propagated to the offshore area near the southeast coast of Taiwan, the semi-elliptic eyewall was built up at the second and third quad- rants. -
1 29Th Conference on Hurricanes and Tropical Meteorology, 10–14 May 2010, Tucson, Arizona
9C.3 ASSESSING THE IMPACT OF TOTAL PRECIPITABLE WATER AND LIGHTNING ON SHIPS FORECASTS John Knaff* and Mark DeMaria NOAA/NESDIS Regional and Mesoscale Meteorology Branch, Fort Collins, Colorado John Kaplan NOAA/AOML Hurricane Research Division, Miami, Florida Jason Dunion CIMAS, University of Miami – NOAA/AOML/HRD, Miami, Florida Robert DeMaria CIRA, Colorado State University, Fort Collins, Colorado 1. INTRODUCTION 1 would be anticipated from the Clausius-Clapeyron relationships (Stephens 1990). This study is motivated by the potential of two The TPW is typically estimated by its rather unique datasets, namely measures of relationship with certain passive microwave lightning activity and Total Precipitable Water channels ranging from 19 to 37 GHz (Kidder and (TPW), and their potential for improving tropical Jones 2007). These same channels, particularly cyclone intensity forecasts. 19GHz in the inner core region, have been related The plethora of microwave imagers in low to tropical cyclone intensity change (Jones et al earth orbit the last 15 years has made possible the 2006). TPW fields also offer an excellent regular monitoring of water vapor and clouds over opportunity to monitor real-time near core the earth’s oceanic areas. One product that has atmospheric moisture, which like rainfall (i.e. much utility for short-term weather forecasting is 19GHz) is related to intensity changes as the routine monitoring of total column water vapor modeling studies of genesis/formation suggest or TPW. that saturation of the atmospheric column is In past studies lower environmental moisture coincident or precede rapid intensification (Nolan has been shown to inhibit tropical cyclone 2007). development and intensification (Dunion and In addition to the availability of real-time TPW Velden 2004; DeMaria et al 2005, Knaff et al data, long-range lightning detection networks now 2005). -
Florida Housing Coalition Hurricane Member Update Webinar May 1, 2020 Sponsored by Fannie Mae AGENDA
Florida Housing Coalition Hurricane Member Update Webinar May 1, 2020 Sponsored by Fannie Mae AGENDA • COVID-19 Updates • NOAA, National Hurricane Center, and National Weather Service: Preparing for Hurricane Season COVID-19 SHIP Frequently Asked Questions New Content on Topics Including: • File Documentation • Technical Revisions • Rental Assistance • Mortgage Assistance • Foreclosure Counseling • Reporting COVID SHIP Assistance FAQ File Documentation Question Upcoming COVID-19 Trainings “Implementing Effective Rental Assistance Programs with Federal and State Resources” May 13 at 10:00 am https://attendee.gotowebinar.com/register/7291419462613166863 “COVID-19 SHIP Rent Assistance Implementation" May 18 at 2:00 pm https://attendee.gotowebinar.com/register/7691296448631153675 “COVID-19 SHIP Mortgage Assistance Implementation" May 20 at 2:00 pm https://attendee.gotowebinar.com/register/620374553799087627 Recent COVID-19 Trainings Recordings: • Emergency SHIP Assistance for Renters https://vimeo.com/403418248 • Helping Homeowners with COVID-19 SHIP Emergency Assistance https://vimeo.com/407646578 • Assisting Homeless and Special Needs Populations through COVID-19 https://vimeo.com/405609513 • Virtual SHIP https://vimeo.com/410260129 NOAA, National Hurricane Center, and National Weather Service: Preparing for Hurricane Season Andrew Latto NHC Hurricane Specialist [email protected] Regarding evacuations and planning: • https://www.weather.gov/wrn/2020-hurricane- evacuation Regarding Evacuations and Planning Regarding evacuations and planning: -
Hurricane & Tropical Storm
5.8 HURRICANE & TROPICAL STORM SECTION 5.8 HURRICANE AND TROPICAL STORM 5.8.1 HAZARD DESCRIPTION A tropical cyclone is a rotating, organized system of clouds and thunderstorms that originates over tropical or sub-tropical waters and has a closed low-level circulation. Tropical depressions, tropical storms, and hurricanes are all considered tropical cyclones. These storms rotate counterclockwise in the northern hemisphere around the center and are accompanied by heavy rain and strong winds (NOAA, 2013). Almost all tropical storms and hurricanes in the Atlantic basin (which includes the Gulf of Mexico and Caribbean Sea) form between June 1 and November 30 (hurricane season). August and September are peak months for hurricane development. The average wind speeds for tropical storms and hurricanes are listed below: . A tropical depression has a maximum sustained wind speeds of 38 miles per hour (mph) or less . A tropical storm has maximum sustained wind speeds of 39 to 73 mph . A hurricane has maximum sustained wind speeds of 74 mph or higher. In the western North Pacific, hurricanes are called typhoons; similar storms in the Indian Ocean and South Pacific Ocean are called cyclones. A major hurricane has maximum sustained wind speeds of 111 mph or higher (NOAA, 2013). Over a two-year period, the United States coastline is struck by an average of three hurricanes, one of which is classified as a major hurricane. Hurricanes, tropical storms, and tropical depressions may pose a threat to life and property. These storms bring heavy rain, storm surge and flooding (NOAA, 2013). The cooler waters off the coast of New Jersey can serve to diminish the energy of storms that have traveled up the eastern seaboard. -
Downloaded 10/05/21 07:00 AM UTC 3074 MONTHLY WEATHER REVIEW VOLUME 145
AUGUST 2017 H A Z E L T O N E T A L . 3073 Analyzing Simulated Convective Bursts in Two Atlantic Hurricanes. Part I: Burst Formation and Development a ANDREW T. HAZELTON Department of Earth, Ocean and Atmospheric Science, The Florida State University, Tallahassee, Florida ROBERT F. ROGERS NOAA/AOML/Hurricane Research Division, Miami, Florida ROBERT E. HART Department of Earth, Ocean and Atmospheric Science, The Florida State University, Tallahassee, Florida (Manuscript received 15 July 2016, in final form 21 April 2017) ABSTRACT Understanding the structure and evolution of the tropical cyclone (TC) inner core remains an elusive challenge in tropical meteorology, especially the role of transient asymmetric features such as localized strong updrafts known as convective bursts (CBs). This study investigates the formation of CBs and their role in TC structure and evolution using high-resolution simulations of two Atlantic hurricanes (Dean in 2007 and Bill in 2009) with the Weather Research and Forecasting (WRF) Model. Several different aspects of the dynamics and thermodynamics of the TC inner-core region are investigated with respect to their influence on TC convective burst development. Composites with CBs show stronger radial inflow in the lowest 2 km, and stronger radial outflow from the eye to the eyewall around z 5 2–4 km, than composites without CBs. Asymmetric vorticity associated with eyewall mesovortices appears to be a major factor in some of the radial flow anomalies that lead to CB development. The anomalous outflow from these mesovortices, along with outflow from supergradient parcels above the boundary layer, favors low-level convergence and also appears to mix high-ue air from the eye into the eyewall. -
High-Resolution Hurricane Forecasts
H u r r i c a n e p r e d i c t i o n High-Resolution Hurricane Forecasts Widely varying scales of atmospheric motion make it extremely difficult to predict hurricane intensity, even after decades of research. A new model capable of resolving a hurricane’s deep convection motions was tested on a large sample of Atlantic tropical cyclones. Results show that using finer resolution can improve storm intensity predictions. redicting a hurricane’s intensity re- Most current weather prediction uses grid-based mains a daunting challenge even after rather than spectral-based models (such as Fourier four decades of research. The intrinsic or some other basis function).1 Statistical analy- difficulties lie in the vast range of spa- sis of energy spectra reveal that motions with Ptial and temporal scales of atmospheric motions scales smaller than approximately six to seven grid that affect tropical cyclone intensity. The range of points aren’t well resolved.2 Therefore, the mini- spatial scales is literally millimeters to 1,000 kilo- mum resolvable physical length scales are nearly meters or more. 1 km horizontally and perhaps 300 m vertically. Atmospheric dynamical models must account Given current computing capability, however, for all these scales simultaneously. Being a non- timely numerical forecasts must be run on much linear system, these scales can interact. Although coarser grids. forecasters must make approximations to keep What does this mean for hurricane forecasts? computations finite, there’s a continued push for We believe that it’s important to resolve clouds— finer resolution to capture as many of these scales at least the largest cumulonimbus-producing as possible. -
11B-01 Polygonal Eyewall Asymmetries During the Rapid Intensification of Hurricane Michael (2018)
11B-01 POLYGONAL EYEWALL ASYMMETRIES DURING THE RAPID INTENSIFICATION OF HURRICANE MICHAEL (2018) Ting-Yu Cha1*, Michael M. Bell1, Wen-Chau Lee2, Alexander J. DesRosiers1 1Colorado State University, Fort Collins, Colorado 2National Center for Atmospheric Research, Boulder, Colorado 1. INTRODUCTION Hurricane Michael (2018) was the first axisymmetric and asymmetric tangential winds Category 5 hurricane to make landfall in the (Jou et al. 2008; Cha and Bell 2019). United States since Hurricane Andrew (1992) and Analyses of Hurricane Michael (2018) caused extensive damage in Florida and Georgia demonstrate the first observation of high-order (Beven et al. 2019). Satellite and radar imagery wave propagation using tangential wind showed evidence of an evolving polygonal asymmetries as a proxy for the PV signal. The eyewall as Michael underwent rapid results show that the propagation speeds of the intensification (RI) during its approach to Florida. waves are consistent with linear wave theory on Polygonal eyewalls are hypothesized to be the a vortex and help to provide new insight into result of asymmetric vorticity dynamics internal to physical mechanisms contributing to TC rapid the storm that can modulate TC structure and intensification. intensity through counter-propagating vortex Rossby waves (VRWs) that redistribute eyewall 2. DATA AND METHODOLOGY potential vorticity (PV) and angular momentum Hurricane Michael was within the NEXRAD and form mesovortices (Hendricks et al. 2012; KEVX ground-based radar surveillance range Kuo et al. 1999,2016; Muramatsu 1986; Schubert during its rapid intensification (RI), and its et al. 1999, Lee and Wu 2019). TC internal intensity reached category 5 (140 kt) at the time dynamics are a primary factor impacting the rate of landfall around 1730 UTC (Fig. -
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HURRICANE FRED (2015) Cape Verde’s First Hurricane in Modern Times: Observations, Impacts, and Lessons Learned GREGORY S. JENKINS, ESTER BRITO, EMANUEL SOARES, SEN CHIAO, JOSE PIMENTA LIMA, BENVENDO TAVARES, ANGELO CARDOSO, FRANCISCO EVORA, AND MARIA MONTEIRO Surface and satellite observations along with WRF Model forecasts provide a unique view of Hurricane Fred, the first to strike Cape Verde in 124 years. ropical cyclones remain the deadliest form of inhibiting factor to development because of dry air, short- to medium-range weather hazards (Obasi positive stability, and wind shear (Evan et al. 2006). T1994). While track forecasts have improved signif- However, dust associated with the SAL may also icantly, tropical cyclogenesis and rapid intensification potentially lead to convective invigoration through remain challenges and have been the focus of recent microphysical processes (Koren et al. 2005; Jenkins field campaigns (Montgomery et al. 2012; Braun et al. et al. 2008; Rosenfeld et al. 2012). While infrequent, 2013; Rogers et al. 2013). In the extreme eastern At- tropical depressions and storms have formed near lantic, tropical cyclones are less frequent than in the the Cape Verde islands, as was the case during the central and western Atlantic because the waters are NASA African Monsoon Multidisciplinary Analysis cooler and the Saharan air layer (SAL) can act as an (NAMMA) campaign with Tropical Depression 8 and Tropical Storm (TS) Debby (Zipser et al. 2009; Zawislak and Zipser 2010). AFFILIATIONS: JENKINS—Department of Meteorology, The Cape Verde is located approximately 400 miles Pennsylvania State University, University Park, Pennsylvania; (~644 km) to the west of Senegal. It comprises 10 BRITO, SOARES, PIMENTA LIMA, TAVARES, CARDOSO, EVORA, AND islands, with significant variations in climate and land- MONTEIRO—Institute for Meteorology and Geophysics, Ilha do Sal, scape among the islands. -
Hurricane Names: a Bunch of Hot Air?
Weather and Climate Extremes 12 (2016) 80–84 Contents lists available at ScienceDirect Weather and Climate Extremes journal homepage: www.elsevier.com/locate/wace Hurricane names: A bunch of hot air? Gary Smith n Department of Economics, Pomona College, United States article info abstract Article history: It has been argued that female-named hurricanes are deadlier because people do not take them ser- Received 7 July 2015 iously. However, this conclusion is based on a questionable statistical analysis of a narrowly defined data Received in revised form set. The reported relationship is not robust in that it is not confirmed by a straightforward analysis of 10 November 2015 more inclusive data or different data. Accepted 22 November 2015 & 2015 Elsevier B.V. This is an open access article under the CC BY-NC-ND license Available online 28 November 2015 (http://creativecommons.org/licenses/by-nc-nd/4.0/). Keywords: Hurricanes Data grubbing Sexism Jung, Shavitt, Viswanathan, and Hilbe (2014) argue that people depression (less than 39 mph), tropical storm (39–73 mph), hur- do not take hurricanes with female names seriously and are con- ricane (more than 73 mph), and major hurricane (more than sequently underprepared and more likely to be killed. The authors 110 mph). Tropical storms and hurricanes are generally given report that this “hazardous form of implicit sexism” is supported names like Hurricane Sandy, but tropical depressions are not. by their analysis of 92 hurricanes that hit the United States be- Jung et al. (2014) examine a narrowly defined dataset: U.S. tween 1950 and 2012.