Extended Range Forecast of Atlantic Seasonal Hurricane Activity and Landfall Strike Probability for 2021
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Subtropical Storms in the South Atlantic Basin and Their Correlation with Australian East-Coast Cyclones
2B.5 SUBTROPICAL STORMS IN THE SOUTH ATLANTIC BASIN AND THEIR CORRELATION WITH AUSTRALIAN EAST-COAST CYCLONES Aviva J. Braun* The Pennsylvania State University, University Park, Pennsylvania 1. INTRODUCTION With the exception of warmer SST in the Tasman Sea region (0°−60°S, 25°E−170°W), the climate associated with South Atlantic ST In March 2004, a subtropical storm formed off is very similar to that associated with the coast of Brazil leading to the formation of Australian east-coast cyclones (ECC). A Hurricane Catarina. This was the first coastal mountain range lies along the east documented hurricane to ever occur in the coast of each continent: the Great Dividing South Atlantic basin. It is also the storm that Range in Australia (Fig. 1) and the Serra da has made us reconsider why tropical storms Mantiqueira in the Brazilian Highlands (Fig. 2). (TS) have never been observed in this basin The East Australia Current transports warm, although they regularly form in every other tropical water poleward in the Tasman Sea tropical ocean basin. In fact, every other basin predominantly through transient warm eddies in the world regularly sees tropical storms (Holland et al. 1987), providing a zonal except the South Atlantic. So why is the South temperature gradient important to creating a Atlantic so different? The latitudes in which TS baroclinic environment essential for ST would normally form is subject to 850-200 hPa formation. climatological shears that are far too strong for pure tropical storms (Pezza and Simmonds 2. METHODOLOGY 2006). However, subtropical storms (ST), as defined by Guishard (2006), can form in such a. -
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. -
Lecture 15 Hurricane Structure
MET 200 Lecture 15 Hurricanes Last Lecture: Atmospheric Optics Structure and Climatology The amazing variety of optical phenomena observed in the atmosphere can be explained by four physical mechanisms. • What is the structure or anatomy of a hurricane? • How to build a hurricane? - hurricane energy • Hurricane climatology - when and where Hurricane Katrina • Scattering • Reflection • Refraction • Diffraction 1 2 Colorado Flood Damage Hurricanes: Useful Websites http://www.wunderground.com/hurricane/ http://www.nrlmry.navy.mil/tc_pages/tc_home.html http://tropic.ssec.wisc.edu http://www.nhc.noaa.gov Hurricane Alberto Hurricanes are much broader than they are tall. 3 4 Hurricane Raymond Hurricane Raymond 5 6 Hurricane Raymond Hurricane Raymond 7 8 Hurricane Raymond: wind shear Typhoon Francisco 9 10 Typhoon Francisco Typhoon Francisco 11 12 Typhoon Francisco Typhoon Francisco 13 14 Typhoon Lekima Typhoon Lekima 15 16 Typhoon Lekima Hurricane Priscilla 17 18 Hurricane Priscilla Hurricanes are Tropical Cyclones Hurricanes are a member of a family of cyclones called Tropical Cyclones. West of the dateline these storms are called Typhoons. In India and Australia they are called simply Cyclones. 19 20 Hurricane Isaac: August 2012 Characteristics of Tropical Cyclones • Low pressure systems that don’t have fronts • Cyclonic winds (counter clockwise in Northern Hemisphere) • Anticyclonic outflow (clockwise in NH) at upper levels • Warm at their center or core • Wind speeds decrease with height • Symmetric structure about clear "eye" • Latent heat from condensation in clouds primary energy source • Form over warm tropical and subtropical oceans NASA VIIRS Day-Night Band 21 22 • Differences between hurricanes and midlatitude storms: Differences between hurricanes and midlatitude storms: – energy source (latent heat vs temperature gradients) - Winter storms have cold and warm fronts (asymmetric). -
Climate Early Warning System Feasibility Report: Early Warning Systems and Hazard Prediction
United Nations Environment Programme Climate Early Warning System Feasibility Report: Early Warning Systems and Hazard Prediction March 2012 Dr. Zinta Zommers University of Oxford 1 Table of Contents 1 INTRODUCTION AND PURPOSE ....................................................................................................................... 3 2. METHODOLOGY................................................................................................................................................. 6 3. CURRENT EARLY WARNING SYSTEMS.......................................................................................................... 8 3.1. COMPONENTS OF EWS ...................................................................................................................... 8 3.2. KEY ACTORS IN EWS......................................................................................................................... 9 3.3. EWS BY NATION .............................................................................................................................. 10 3.4. EWS BY HAZARD............................................................................................................................. 15 3.4.1. Drought.......................................................................................................................................... 15 3.4.2. Famine........................................................................................................................................... 20 3.4.3. Fire................................................................................................................................................ -
Tropical-Cyclone Forecasting: a Worldwide Summary of Techniques
John L. McBride and Tropical-Cyclone Forecasting: Greg J. Holland Bureau of Meteorology Research Centre, A Worldwide Summary Melbourne 3001, of Techniques and Australia Verification Statistics Abstract basis for discussion at particular sessions planned for the work- shop. Replies to this questionnaire were received from 16 of- Questionnaire replies from forecasters in 16 tropical-cyclone warning fices. These are listed in Table 1, grouped according to their centers are summarized to provide an overview of the current state of ocean basins. Encouraged by the high information content of the science in tropical-cyclone analysis and forecasting. Information is tabulated on the data sources and techniques used, on their role and these responses, the authors sent a second questionnaire on the perceived usefulness, and on the levels of verification and accuracy of analysis and forecasting of cyclone position and motion. Re- cyclone forecasting. plies to this were received from 13 of the listed offices. This paper tabulates and syntheses information provided on the following aspects of tropical-cyclone forecasting: 1) the techniques used; 2) the level of verification; and 3) the level 1. Introduction of accuracy of analyses and forecasts. Separate sections cover forecasting of cyclone formation; analyzing cyclone structure Tropical cyclones are the major severe weather hazard for a and intensity; forecasting structure and intensity; analyzing cy- large "slice" of mankind. The Bangladesh cyclones of 1970 and 1985, Hurricane Camille (USA, 1969) and Cyclone Tracy (Australia, 1974) to name just four, would figure prominently TABLE 1. Forecast offices from which unofficial replies were re- in any list of major natural disasters of this century. -
Chapter 2.1.3, Has Both Unique and Common Features That Relate to TC Internal Structure, Motion, Forecast Difficulty, Frequency, Intensity, Energy, Intensity, Etc
Chapter Two Charles J. Neumann USNR (Retired) U, S. National Hurricane Center Science Applications International Corporation 2. A Global Tropical Cyclone Climatology 2.1 Introduction and purpose Globally, seven tropical cyclone (TC) basins, four in the Northern Hemisphere (NH) and three in the Southern Hemisphere (SH) can be identified (see Table 1.1). Collectively, these basins annually observe approximately eighty to ninety TCs with maximum winds 63 km h-1 (34 kts). On the average, over half of these TCs (56%) reach or surpass the hurricane/ typhoon/ cyclone surface wind threshold of 118 km h-1 (64 kts). Basin TC activity shows wide variation, the most active being the western North Pacific, with about 30% of the global total, while the North Indian is the least active with about 6%. (These data are based on 1-minute wind averaging. For comparable figures based on 10-minute averaging, see Table 2.6.) Table 2.1. Recommended intensity terminology for WMO groups. Some Panel Countries use somewhat different terminology (WMO 2008b). Western N. Pacific terminology used by the Joint Typhoon Warning Center (JTWC) is also shown. Over the years, many countries subject to these TC events have nurtured the development of government, military, religious and other private groups to study TC structure, to predict future motion/intensity and to mitigate TC effects. As would be expected, these mostly independent efforts have evolved into many different TC related global practices. These would include different observational and forecast procedures, TC terminology, documentation, wind measurement, formats, units of measurement, dissemination, wind/ pressure relationships, etc. Coupled with data uncertainties, these differences confound the task of preparing a global climatology. -
ANNUAL SUMMARY Atlantic Hurricane Season of 2005
MARCH 2008 ANNUAL SUMMARY 1109 ANNUAL SUMMARY Atlantic Hurricane Season of 2005 JOHN L. BEVEN II, LIXION A. AVILA,ERIC S. BLAKE,DANIEL P. BROWN,JAMES L. FRANKLIN, RICHARD D. KNABB,RICHARD J. PASCH,JAMIE R. RHOME, AND STACY R. STEWART Tropical Prediction Center, NOAA/NWS/National Hurricane Center, Miami, Florida (Manuscript received 2 November 2006, in final form 30 April 2007) ABSTRACT The 2005 Atlantic hurricane season was the most active of record. Twenty-eight storms occurred, includ- ing 27 tropical storms and one subtropical storm. Fifteen of the storms became hurricanes, and seven of these became major hurricanes. Additionally, there were two tropical depressions and one subtropical depression. Numerous records for single-season activity were set, including most storms, most hurricanes, and highest accumulated cyclone energy index. Five hurricanes and two tropical storms made landfall in the United States, including four major hurricanes. Eight other cyclones made landfall elsewhere in the basin, and five systems that did not make landfall nonetheless impacted land areas. The 2005 storms directly caused nearly 1700 deaths. This includes approximately 1500 in the United States from Hurricane Katrina— the deadliest U.S. hurricane since 1928. The storms also caused well over $100 billion in damages in the United States alone, making 2005 the costliest hurricane season of record. 1. Introduction intervals for all tropical and subtropical cyclones with intensities of 34 kt or greater; Bell et al. 2000), the 2005 By almost all standards of measure, the 2005 Atlantic season had a record value of about 256% of the long- hurricane season was the most active of record. -
Hurricane & Tornado Risks in June
June 4, 2021 Hurricane & Tornado Risks in June · Several changes in the weather typically occur in June across the Lower 48. Tropical Development · Atlantic hurricane season officially starts June 1, although it has started early the last seven years, including this year. · On average in the Atlantic Basic, one named storm forms every one to two years in June and a hurricane develops about once every five years. · Early in the season, tropical systems tend to form close to the U.S. and often affect the Southeastern U.S., the western Caribbean and parts of Central America. Rainfall, rather than wind, is usually the biggest concern with June tropical cyclones. Tornado Risks · June is typically an active month for tornadoes. · Tornadoes can happen just about anywhere in the Lower 48 in June, given the widespread warmth and humidity. · Low pressure systems can create the ingredients for severe weather in the Plains and Midwest, in particular. The area at greatest risk of tornadoes in June stretches from central Oklahoma into southwestern Minnesota. · Brief, usually weaker tornadoes often occur near the Gulf Coast during the summer. These are usually caused by sea-breeze thunderstorms and sea breeze collisions closer to the coast. Scattered thunderstorms can also create brief tornadoes across much of the South. · Tropical systems can also bring tornadoes, although they are usually weak and short-lived. · Peak hail activity also occurs in June, according to some studies. The Central and Southern Plains see an increase in hail during the early summer due to the combination of the jet stream, moisture from the Gulf of Mexico and daytime heating. -
A Preliminary Investigation of Derecho-Producing Mcss In
P 3.1 TROPICAL CYCLONE TORNADO RECORDS FOR THE MODERNIZED NWS ERA Roger Edwards1 Storm Prediction Center, Norman, OK 1. INTRODUCTION and BACKGROUND since 1954 was attributable to the weakest (F0) bin of damage rating (Fig. 1). This is the very class of Tornadoes from tropical cyclones (hereafter TCs) tornado that is most common in TC records, and most pose a specialized forecast challenge at time scales difficult to detect in the damage above that from the ranging from days for outlooks to minutes for concurrent or subsequent passage of similarly warnings (Spratt et al. 1997, Edwards 1998, destructive, ambient TC winds. As such, it is possible Schneider and Sharp 2007, Edwards 2008). The (but not quantifiable) that many TC tornadoes have fundamental conceptual and physical tenets of gone unrecorded even in the modern NWS era, due midlatitude supercell prediction, in an ingredients- to their generally ephemeral nature, logistical based framework (e.g., Doswell 1987, Johns and difficulties of visual confirmation, presence of swaths Doswell 1992), fully apply to TC supercells; however, of sparsely populated near-coastal areas (i.e., systematic differences in the relative magnitudes of marshes, swamps and dense forests), and the moisture, instability, lift and shear in TCs (e.g., presence of damage inducers of potentially equal or McCaul 1991) contribute strongly to that challenge. greater impact within the TC envelope. Further, there is a growing realization that some TC tornadoes are not necessarily supercellular in origin (Edwards et al. 2010, this volume). Several major TC tornado climatologies have been published since the 1960s (e.g., Pearson and Sadowski 1965, Hill et al. -
Storms Are Thunderstorms That Produce Tornadoes, Large Hail Or Are Accompanied by High Winds
From February 17 to 19, a severe storm blasted the Lebanese coast with 100- kilometer (60-mile) winds and dropped as much as 2 meters (7 feet) of snow on parts of the country, news sources said. Temperatures dropped to near freezing along the coast, while snowplows struggled to clear the main roadway between Beirut and Damascus. The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite captured this natural-color image on February 20, 2012. Snow covers much of Lebanon, and extends across the border with Syria. Another expanse of snow occurs just north of the Syria-Jordan border. Snow in Lebanon is not uncommon, and the country is home to ski resorts. Still, this fierce storm may have been part of a larger pattern of cold weather in Europe and North Africa. References The Daily Star. (2012, February 18). Lebanon hit by extreme weather conditions. Accessed February 21, 2012. Naharnet. (2012, February 19). Storm subsides after coating Lebanon in snow. Accessed February 21, 2012. NASA image courtesy LANCE/EOSDIS MODIS Rapid Response Team at NASA GSFC. Caption by Michon Scott. Instrument: Terra - MODIS Flooding is the most common of all natural hazards. Each year, more deaths are caused by flooding than any other thunderstorm related hazard. We think this is because people tend to underestimate the force and power of water. Six inches of fast-moving water can knock you off your feet. Water 24 inches deep can carry away most automobiles. Nearly half of all flash flood deaths occur in automobiles as they are swept downstream. -
Hurricanes: a Century of Scientific Progress
Hurricanes: A Century of Scientific Progress Kerry Emanuel Program in Atmospheres, Oceans, and Climate Massachusetts Institute of Technology 1. Introduction In the early 20th century, at the same time that the theories of relativity and quantum mechanics were being developed, there was essentially no basic understanding of the physics of hurricanes. The energy cycle that sustains such storms was not known, nor were the factors that controlled their movement. What was known about the structure and behavior of hurricanes was inferred largely from visual observations of clouds and damage patterns, and it was widely believed that the storm circulation extended upward only a few kilometers. By the end of the century, the structure and behavior of hurricanes had been thoroughly quantified, thanks to rapid technological progress that brought about such wonders as aircraft, radar and satellites, and the basic physics of the storms themselves as well as their intricate substructure had come to be well understood. This new understanding, coupled with the invention and rapid development of the computer, made it possible to forecast the motion of hurricanes with such accuracy that, given modern communications and transportation, loss of life from hurricanes has been virtually eliminated in the developed world. This chapter chronicles the extraordinary progress in the scientific understanding of hurricanes through the 20th century. We begin with a brief review of progress through World War II, which marked an important turning point in the science of meteorology, and continue with an account of the rapid progress made in the first two decades after the war. Section 4 discusses the very influential CISK theory that was developed in the 1960s. -
ESCI 107 – the Atmosphere Lesson 16 – Tropical Cyclones Reading
ESCI 107 – The Atmosphere Lesson 16 – Tropical Cyclones Reading: Meteorology Today, Chapter 15 TROPICAL CYCLONES l A tropical cyclone is a large, low-pressure system that forms over the tropical oceans. l Tropical cyclones are classified by sustained wind speed as o Tropical disturbance – wind less than 25 knots o Tropical Depression (TD) – wind 25 to 34 knots o Tropical storm (TS) – wind 35 to 64 knots o Hurricane (or Typhoon) – wind 65 knots or greater l Sustained winds means winds averaged over a 1-minute period (in U.S.). o It is the sustained wind that is used to classify tropical cyclones, not the gusts. l A typhoon and a hurricane are the exact same thing. They just have different names in different parts of the world. Global numbers ¡ About 80 tropical cyclones per year world-wide reach tropical storm strength ¡ About 50 – 55 each year world-wide reach hurricane/typhoon strength Safir-Simpson Intensity Scale (used in U.S.) Category Max Sustained Wind knots mph 1 64 - 82 74 - 95 2 83 - 95 96 - 110 3 96 - 113 111 - 130 4 114 - 134 131 - 155 5 135 + 156 + ¡ A major hurricane is a Category III or higher. FORMATION l The energy that drives hurricanes is the latent heat of condensation from the thunderstorms that comprise the hurricane. l Therefore, hurricanes can only form over very warm water, where there is plenty of evaporation to feed moisture to the thunderstorms. o Water temperatures must be at least 26.5°C (about 80°F). o The upper ‘mixed layer’ of the ocean must also be relatively deep (at least 45 meters) so that the waves do not mix away the warm water at the surface.