Hurricane Helene Information from NHC Advisory 13, 11:00 AM AST Mon Sep 10, 2018 Helene Is Moving Toward the West-Northwest Near 16 Mph (26 Km/H)
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On the Structure of Hurricane Daisy 1958
NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 48 On the Structure of Hurricane Daisy 1958 ^ 4 & U. S. DEPARTMENT OF COMMERCE Luther H. Hodges, Secretary WEATHER BUREAU F. W. Rolcheldorfoi, Chief NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 48 On the Structure of Hurricane Daisy (1958) by J6se A. Coltfn and Staff National Hurricane Research Project, Miami, Fla. Washington, D. C. October 1961 NATIONAL HURRICANE RESEARCH PROJECT REPORTS Reports by Weather Bureau units, contractors, and ccoperators working on the hurricane problem are preprinted in this series to facilitate immediate distribution of the information among the workers and other interested units. Aa this limited reproduction and distribution in this form do not constitute formal scientific publication, reference to a paper in the series should identify it as a preprinted report. Objectives and basic design of the NHRP. March 1956. No. 1. numerical weather prediction of hurricane motion. July 1956- No. 2. Supplement: Error analysis of prognostic 500-mb. maps made for numerical weather prediction of hurricane motion. March 1957. Rainfall associated with hurricanes. July 1956. No. 3. Some problems involved in the study of storm surges. December 1956. No. h. Survey of meteorological factors pertinent to reduction of loss of life and property in hurricane situations. No. 5. March 1937* A mean atmosphere for the West Indies area. May 1957. No. 6. An index of tide gages and tide gage records for the Atlantic and Gulf coasts of the United States, toy 1957. No. 7. No. 8. PartlT HurrlcaneVand the sea surface temperature field. Part II. The exchange of energy between the sea and the atmosphere in relation to hurricane behavior. -
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. -
Hurricane Florence
Hurricane Florence: Powerful and relentless storm batters the Carolinas (English I Honors) Required Annotations Student-Created Annotations Summary / Questions / Reflection Student-created Required (bold) WILMINGTON, North Carolina — Hurricane Florence lumbered ashore in North Carolina with howling winds of 90 miles per hour (mph) and a terrifying storm surge early on Friday, September 14, splintering buildings and trapping hundreds of people in high water as it settled in for what could be a long and extraordinarily destructive drenching. More than 60 people had to be pulled from a collapsing cinderblock motel at the height of the storm. Hundreds more had to be rescued elsewhere from rising waters. And others could only hope someone would come for them. "WE ARE COMING TO GET YOU," the city of New Bern tweeted around 2 a.m. "You may need to move up to the second story, or to your attic, but WE ARE COMING TO GET YOU." As Florence pounded away, it unloaded heavy rain, flattened trees, chewed away at roads and knocked out power to more than a half-million homes and businesses. Ominously, forecasters said the onslaught on the North Carolina-South Carolina coast would last for hours and hours because the hurricane had come almost to a dead stop at just 3 mph as of midday Friday. North Carolina Governor Roy Cooper said the hurricane was "wreaking havoc" on the coast and could wipe out entire communities as it makes its "violent grind across our state for days." He called the rain an event that comes along only once every 1,000 years. -
HURRICANE ISAAC (AL092018) 7–15 September 2018
NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT HURRICANE ISAAC (AL092018) 7–15 September 2018 David A. Zelinsky National Hurricane Center 30 January 2019 SUOMI-NPP/VIIRS 1625 UTC 10 SEPTEMBER 2018 TRUE COLOR IMAGE OF ISAAC WHILE IT WAS A HURRICANE. IMAGE COURTESY OF NASA WORLDVIEW. Isaac was a category 1 hurricane (on the Saffir-Simpson Hurricane Wind Scale) that formed over the east-central tropical Atlantic and moved westward. The cyclone weakened and passed through the Lesser Antilles as a tropical storm, causing locally heavy rain and flooding. Hurricane Isaac 2 Hurricane Isaac 7–15 SEPTEMBER 2018 SYNOPTIC HISTORY Isaac developed from a tropical wave that moved off the west coast of Africa on 2 September. A broad area of low pressure was already present when the convectively active wave moved over the eastern Atlantic, and the low gradually consolidated over the next several days while the wave moved steadily westward. A concentrated burst of deep convection initiated late on 6 September and led to the formation of a well-defined center, marking the development of a tropical depression by 1200 UTC 7 September a little more than 600 n mi west of the Cabo Verde Islands. Weak steering flow caused the depression to move very little while moderate easterly wind shear prevented it from strengthening for the first 24 h following formation. The shear decreased the next morning, and the cyclone reached tropical-storm strength by 1200 UTC 8 September. The “best track” chart of Isaac’s path is given in Fig. 1, with the wind and pressure histories shown in Figs. -
Criteria for a Standard Project Northeaster for New England North of Cape Cod
•V-'v';J nagyiwraH ^r—— .Al 3°) PflSt r„y REPORT NO. 68 Criteria for a Standard Project Northeaster for New England North of Cape Cod • •• U. S. DEPARTMENT OF COMMERCE Luther H. Hodges, Secretary WEATHER BUREAU Robert M. White, Chief • NATIONAL HURRICANE RESEARCH PROJECT REPORT NO. 68 Criteria for a Standard Project Northeaster for New England North of Cape Cod by Kendall R. Peterson, Hugo V. Goodyear, and Staff Hydrometeorological Section, Hydrologic Services Division, Washington, D. C. Washington, D. C. UlfiMOl DbDIHSb March 1964 NATIONAL HURRICANE RESEARCH PROJECT REPORTS Reports by Weather Bureau units, contractors, and cooperators working on the hurricane problem are preprinted in this series to facilitate immediate distribution of the information among the workers and other interested units. As this limited reproduction and distribution in this form do not constitute formal scientific publication, reference to a paper in the series should identify it as a preprinted report. No. 1. Objectives and basic design of the NHRP. March 1936. No. 2. Numerical weather prediction of hurricane motion. July 1956. Supplement: Error analysis of prognostic 300-mb. maps made for numerical weather prediction of hurricane motion. March 1937. No. 3« Rainfall associated with hurricanes. July 1956. No. U. Some problems involved in the study of storm surges. December 1936. No. 3* Survey of meteorological factors pertinent to reduction of loss of life and property in hurricane situations. March 1937. No. 6. A mean atmosphere for the West Indies area. May 1937* No. 7. An index of tide' gages and tide gage records for the Atlantic and Gulf coasts of the United States. -
Report of the Annual Meeting of the Directors of Meteorological Services
C A R I B B E A N M E T E O R O L O G I C A L O R G A N I Z A T I O N REPORT OF THE ANNUAL MEETING OF DIRECTORS OF METEOROLOGICAL SERVICES St. Mary’s, ANTIGUA AND BARBUDA 4 DECEMBER 2006 DMS2006 Page 1 INTRODUCTION 1.1 At the kind invitation of the Government of Antigua and Barbuda, the 46th annual Meeting of Directors of Meteorological Services was held at the Jolly Beach Resort, Bolans Village, Antigua and Barbuda, on Monday 4th December 2006 under the Chairmanship of Mr Tyrone Sutherland, Coordinating Director of the Caribbean Meteorological Organisation (CMO). The meeting was addressed by Ms. Elaine Carter, Permanent Secretary, Ministry of Tourism and Civil Aviation who welcomed the participants to Antigua and Barbuda. She expressed the hope that participants would get an opportunity to see more of the Island. She also indicated that she was particularly interested in hearing more about the CMO Radar Project and plans for CWC 2007. Ms. Carter stated that she was especially pleased that the Meeting was being convened during Tourism Week in Antigua and Barbuda. 1.2 A list of participants and observers attending the Meeting is attached as Annex I to this Report and a copy of the Agenda adopted by the Meeting is attached as Annex II to this Report. THE 2006 HURRICANE SEASON (Agenda Item 2) 2.1 The 2006 Hurricane Season was a near-normal season with nine (9) named storms, five (5) hurricanes and two (2) intense hurricanes. -
An Eye on the Storm Integrating a Wealth of Data for Quickly Advancing the Physical Understanding and Forecasting of Tropical Cyclones Svetla M
Article An Eye on the Storm Integrating a Wealth of Data for Quickly Advancing the Physical Understanding and Forecasting of Tropical Cyclones Svetla M. Hristova-Veleva, P. Peggy Li, Brian Knosp, Quoc Vu, F. Joseph Turk, William L. Poulsen, Ziad Haddad, Bjorn Lambrigtsen, Bryan W. Stiles, Tsae-Pyng Shen, Downloaded from http://journals.ametsoc.org/bams/article-pdf/101/10/E1718/5011864/bamsd190020.pdf by NOAA Central Library user on 02 November 2020 Noppasin Niamsuwan, Simone Tanelli, Ousmane Sy, Eun-Kyoung Seo, Hui Su, Deborah G. Vane, Yi Chao, Philip S. Callahan, R. Scott Dunbar, Michael Montgomery, Mark Boothe, Vijay Tallapragada, Samuel Trahan, Anthony J. Wimmers, Robert Holz, Jeffrey S. Reid, Frank Marks, Tomislava Vukicevic, Saiprasanth Bhalachandran, Hua Leighton, Sundararaman Gopalakrishnan, Andres Navarro, and Francisco J. Tapiador ABSTRACT: Tropical cyclones (TCs) are among the most destructive natural phenomena with huge societal and economic impact. They form and evolve as the result of complex multiscale processes and nonlinear interactions. Even today the understanding and modeling of these processes is still lacking. A major goal of NASA is to bring the wealth of satellite and airborne observations to bear on addressing the unresolved scientific questions and improving our forecast models. Despite their significant amount, these observations are still underutilized in hurricane research and operations due to the complexity associated with finding and bringing together semicoincident and semi- contemporaneous multiparameter -
2018 Climate Summary
& ~ Hurricane Season Review ~ Meteorological Department St. Maarten Modesta Drive # 12, Simpson Bay (721) 545-4226 www.meteosxm.com MDS Climatological Summary 2018 The information contained in this Climatological Summary must not be copied in part or any form, or communicated for the use of any other party without the expressed written permission of the Meteorological Department St. Maarten. All data and observations were recorded at the Princess Juliana International Airport. This document is published by the Meteorological Department St. Maarten, and a digital copy is available on our website. Prepared by: Sheryl Etienne-Leblanc Published by: Meteorological Department St. Maarten Modesta Drive # 12, Simpson Bay St. Maarten, Dutch Caribbean Telephone: (721) 545-4226 Website: www.meteosxm.com E-mail: [email protected] www.facebook.com/sxmweather www.twitter.com/@sxmweather MDS © May 2019 Page 2 of 29 MDS Climatological Summary 2018 Table of Contents Introduction.............................................................................................................. 4 Island Climatology……............................................................................................. 5 About Us……………………………………………………………………………..……….……………… 6 2018 Hurricane Season Summary…………………………………………………………………………………………….. 8 Local Effects...................................................................................................... 9 Summary Table ............................................................................................... -
September Weather History for the 1St - 30Th
SEPTEMBER WEATHER HISTORY FOR THE 1ST - 30TH AccuWeather Site Address- http://forums.accuweather.com/index.php?showtopic=7074 West Henrico Co. - Glen Allen VA. Site Address- (Ref. AccWeather Weather History) -------------------------------------------------------------------------------------------------------- -------------------------------------------------------------------------------------------------------- AccuWeather.com Forums _ Your Weather Stories / Historical Storms _ Today in Weather History Posted by: BriSr Sep 1 2008, 11:37 AM September 1 MN History 1807 Earliest known comprehensive Minnesota weather record began near Pembina. The temperature at midday was 86 degrees and a "strong wind until sunset." 1894 The Great Hinckley Fire. Drought conditions started a massive fire that began near Mille Lacs and spread to the east. The firestorm destroyed Hinckley and Sandstone and burned a forest area the size of the Twin City Metropolitan Area. Smoke from the fires brought shipping on Lake Superior to a standstill. 1926 This was perhaps the most intense brief thunderstorm ever in downtown Minneapolis. 1.02 inches of rain fell in six minutes, starting at 2:59pm in the afternoon according to the Minneapolis Weather Bureau. The deluge, accompanied with winds of 42mph, caused visibility to be reduced to a few feet at times and stopped all streetcar and automobile traffic. At second and sixth street in downtown Minneapolis rushing water tore a manhole cover off and a geyser of water spouted 20 feet in the air. Hundreds of wooden paving blocks were uprooted and floated onto neighboring lawns much to the delight of barefooted children seen scampering among the blocks after the rain ended. U.S. History # 1897 - Hailstone drifts six feet deep were reported in Washington County, IA. -
2017 North Atlantic Hurricane Season
Tropical cyclones in 2018 Joanne Camp RMetS Understanding the Weather of 2018 23 March 2019 www.metoffice.gov.uk © Crown Copyright 2017, Met Office Global tropical cyclone activity in 2018 Southern Western Pacific Eastern Pacific North Atlantic hemisphere 2017/18 • Above-average • Most active • Above average number of typhoons hurricane season on • Below-average (13) record • >$33 billion damage season • Notable storms: • Notable storms: • Notable storms: • Notable storms: Yutu (October 2018) Lane (Hawaii, Aug Florence (Sep 2018), Gita (February 2018) and Mangkhut 2018), Willa (Mexico, Michael (Oct 2018) (Philippines, Sep 2018) October 2018) NASA NASA Reuters BBC News North Indian Ocean Most active season since 1992 • 7 cyclones Notable storms: Sagar (Somalia, May 2018), Mekunu (Oman, May 2018), Luban (Yemen, Oct 2018). Records: The first time that two cyclones (Luban and Titli) were active in the Bay of Bengal and Arabian Sea at the same time. Records Source: NOAA began in 1960. Cyclones Luban and Titli over the Arabian Sea and the Bay of Bengal. 10 October 2018. 2018 Hurricane Ernesto Season Debby Helene Florence Chris Total storms: 15 Michael - 8 hurricanes (74+ mph) Leslie - 2 major hurricanes (111+ Oscar Joyce mph) Accumulated Cyclone Gordon Energy (ACE) index = 127 Alberto Isaac Most intense: Kirk Nadine Michael (155 mph) Beryl Total damage > $33 billion (winds >156 mph) (winds 39-73 mph) Most notable records…. 1. Florence became the wettest hurricane on record in North and South Carolina 2. Michael was the strongest hurricane to make landfall in the U.S. since Hurricane Andrew in 1992, causing more than $14 billion in damage. -
Climate Overview of Wilmington, NC
National Weather Climate Overview of Wilmington, NC Service Wilmington, NC Temperatures weather.gov/ilm All-time Heat Records 104° on June 27, 1952 103° on June 30, 2012 103° on August 1, 1999 Hottest Month (avg temp) 84.7° in July 2012 Hottest Year (avg temp) Daily record highs 66.5° in 1990 Average highs/lows Avg Number of Days per Year Daily record lows ≥ 80°: 156 ≥ 90°: 46 ≥ 100°: 1 National Weather Service Weather National TEMP DATA Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec ANNUAL All-time Cold Records Highest Ever 82 85 94 95 101 104 103 103 100 98 87 82 104 0° on December 25, 1989 Average High 56.4 59.9 66.4 74.2 80.7 86.9 89.7 88.1 83.7 75.7 68.0 59.3 74.1 Average Temp 46.0 48.9 55.1 62.9 70.4 77.8 81.1 79.7 74.6 65.2 56.7 48.6 63.9 5° on January 21, 1985 Average Low 35.6 37.9 43.8 51.6 60.0 68.7 72.6 71.3 65.6 54.6 45.4 37.8 53.7 5° on February 14, 1899 Lowest Ever 5 5 9 28 35 48 54 55 42 27 16 0 0 Coldest Month (avg temp) Wilmington has a humid subtropical climate with hot summers and cool winters. Summertime heat 35.7° in January 1977 can become excessive, especially when high humidity accompanies hot temperatures. During the Coldest Year (avg temp) spring and summer months, seabreezes originating from the ocean to the east and south bring 61.0° in 1981 cooler air onshore during most afternoons. -
The Water Budget of a Hurricane As Dependent on Its Movement
The water vapor budget of a hurricane as dependent on its movement Anastassia M. Makarieva1,2,∗ Victor G. Gorshkov1,2, Andrei V. Nefiodov1, Alexander V. Chikunov3,4, Douglas Sheil5, Antonio Donato Nobre6, and Bai-Lian Li2 1Theoretical Physics Division, Petersburg Nuclear Physics Institute, 188300 Gatchina, St. Petersburg, Russia. 2USDA-China MOST Joint Research Center for AgroEcology and Sustainability, University of California, Riverside 92521-0124, USA. 3Institute of World Ideas, Udaltsova street 1A, 119415 Moscow, Russia. 4Princeton Institute of Life Sciences, Princeton, USA. 5Norwegian University of Life Sciences, As,˚ Norway. 6Centro de Ciˆencia do Sistema Terrestre INPE, S˜ao Jos´edos Campos SP 12227-010, Brazil. Abstract Despite the dangers associated with tropical cyclones and their rainfall, the origins of storm moisture remains unclear. Existing studies have focused on the region 40-400 km from the cyclone center. It is known that the rainfall within this area cannot be explained by local processes alone but requires imported moisture. Nonetheless, the dynamics of this imported moisture appears unknown. Here, con- sidering a region up to three thousand kilometers from storm center, we analyze precipitation, atmospheric moisture and movement velocities for North Atlantic hurricanes. Our findings indicate that even over such large areas a hurricane’s rain- fall cannot be accounted for by concurrent evaporation. We propose instead that a hurricane consumes pre-existing atmospheric water vapor as it moves. The prop- agation velocity of the cyclone, i.e. the difference between its movement velocity and the mean velocity of the surrounding air (steering flow), determines the water vapor budget. Water vapor available to the hurricane through its movement makes the hurricane self-sufficient at about 700 km from the hurricane center obviating the need to concentrate moisture from greater distances.