The Atlantic Hurricane Season Summary – 2015
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Historical Changes in the Mississippi-Alabama Barrier Islands and the Roles of Extreme Storms, Sea Level, and Human Activities
HISTORICAL CHANGES IN THE MISSISSIPPI-ALABAMA BARRIER ISLANDS AND THE ROLES OF EXTREME STORMS, SEA LEVEL, AND HUMAN ACTIVITIES Robert A. Morton 88∞46'0"W 88∞44'0"W 88∞42'0"W 88∞40'0"W 88∞38'0"W 88∞36'0"W 88∞34'0"W 88∞32'0"W 88∞30'0"W 88∞28'0"W 88∞26'0"W 88∞24'0"W 88∞22'0"W 88∞20'0"W 88∞18'0"W 30∞18'0"N 30∞18'0"N 30∞20'0"N Horn Island 30∞20'0"N Petit Bois Island 30∞16'0"N 30∞16'0"N 30∞18'0"N 30∞18'0"N 2005 2005 1996 Dauphin Island 1996 2005 1986 1986 30∞16'0"N Kilometers 30∞14'0"N 0 1 2 3 4 5 1966 30∞16'0"N 1950 30∞14'0"N 1950 Kilometers 1917 0 1 2 3 4 5 1917 1848 1849 30∞14'0"N 30∞14'0"N 30∞12'0"N 30∞12'0"N 30∞12'0"N 30∞12'0"N 30∞10'0"N 30∞10'0"N 88∞46'0"W 88∞44'0"W 88∞42'0"W 88∞40'0"W 88∞38'0"W 88∞36'0"W 88∞34'0"W 88∞32'0"W 88∞30'0"W 88∞28'0"W 88∞26'0"W 88∞24'0"W 88∞22'0"W 88∞20'0"W 88∞18'0"W 89∞10'0"W 89∞8'0"W 89∞6'0"W 89∞4'0"W 88∞58'0"W 88∞56'0"W 88∞54'0"W 88∞52'0"W 30∞16'0"N Cat Island Ship Island 30∞16'0"N 2005 30∞14'0"N 1996 30∞14'0"N 1986 Kilometers 1966 0 1 2 3 30∞14'0"N 1950 30∞14'0"N 1917 1848 Fort 2005 Massachusetts 1995 1986 Kilometers 1966 0 1 2 3 30∞12'0"N 1950 30∞12'0"N 1917 30∞12'0"N 30∞12'0"N 1848 89∞10'0"W 89∞8'0"W 89∞6'0"W 89∞4'0"W 88∞58'0"W 88∞56'0"W 88∞54'0"W 88∞52'0"W Open-File Report 2007-1161 U.S. -
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. -
Desoto's Seafood Kitchen
beachin’August 2019 LIFE ON THE ALABAMA GULF COAST LET YOUR STYLE ROAR With Disney’s The Lion King Collection by Pandora © 2019 Pandora Jewelry, LLC • All rights reserved • The Lion King © 2019 Disney DIAMOND JEWELERS GULF SHORES 251-967-4141 DIAMONDJEWELERS.NET 10583120 2 Beachin’ ● August 2019 August 2019 ● Beachin’ 3 4 Beachin’ ● August 2019 August 2019 ● Beachin’ 5 6 Beachin’ ● August 2019 August 2019 ● Beachin’ 7 beachin’ A specialty publication of Gulf Coast Media about the cover contents publisher Parks Rogers Blue skies and the bright summer sun greets Too Close for Comfort [email protected] visitors to Alabama’s Gulf Coast. Kick back and enjoy the beautiful view. Hurricane Barry August 2019 2019 August August beachin’2019 August LIFE ON THE ALABAMA GULF COAST managing editor Photo by Jack Swindle Allison Marlow [email protected] 16 design and layout Paige Marmolejo [email protected] Sands of Time advertising Charter boat fishing begins LouAnn Love [email protected] 251.943.2151 Frank Kustura [email protected] 24 251.923.8129 feature Bethany Randall [email protected] Beach Happenings 251.266.9982 story August events and activities Beachin’ magazine is published Bushwackers at the beach monthly by Gulf Coast Media, 901 N. McKenzie Street, Foley, AL 36535 251.943.2151 Try one or try them all, just don’t Distributed free by The Alabama Gulf Coast Convention & Visitor’s Bureau and at other miss this “must do” summer drink 28 locations throughout Gulf Shores, Orange Beach and Fort Morgan. All rights reserved. Reproduction without permission is prohibited. 10 Nature Gulf Coast Media accepts no responsibility in the guarantee of goods Green Sea Turtles visit Alabama and services advertised herein. -
Hurricane Danny
HURRICANE TRACKING ADVISORY eVENT™ Hurricane Danny Information from NHC Advisory 10, 5:00 PM EDT Thursday August 20, 2015 Danny is moving toward the west-northwest near 10 mph and this general motion is expected to continue into Saturday. Maximum sustained winds have increased to near 80 mph with higher gusts. Some additional strengthening is forecast during the next 24 hours, but a weakening trend is expected to begin after that. Intensity Measures Position & Heading U.S. Landfall (NHC) Max Sustained Wind 80 mph Position Relative to 1030 miles E of the Lesser Speed: (category 1) Land: Antilles Est. Time & Region: n/a Min Central Pressure: 990 mb Coordinates: 13.0 N, 45.7 W Trop. Storm Force Est. Max Sustained Wind 60 miles Bearing/Speed: WNW or 295 degrees at 10 mph n/a Winds Extent: Speed: Forecast Summary The current NHC forecast map (below left) shows Danny moving toward the Lesser Antilles over the next few days at hurricane strength and then weakening to a tropical storm on Sunday. The windfield map (below right) is based on the NHC’s forecast track and shows Danny maintaining category 1 hurricane strength through Sunday, with 74 – 95 mph winds, and then weakening to a tropical storm by Tuesday. To illustrate the uncertainty in Danny’s forecast track, forecast tracks for all current models are shown on the map in pale gray. Forecast Track for Hurricane Danny Forecast Windfield for Hurricane Danny (National Hurricane Center) (Based on NHC at 12:00 UTC) from Kinetic Analysis Corp. Pittsburgh Washington D.C. Cincinnati US ! D Trop Dep Ï TD TS !S Ï Trop Storm Cat 1 !1 Ï Cat 1 Nassau Havana TropicTropic ofof CancerCancer MX CU Santo Domingo DO Port-au-PrinceSan Juan Kingston 08-25 08-24 HN 08-23 Fort-De-France 08-22 NI Castries 08-21 Managua Willemstad Caracas 08-20 CR CR Maracaibo Port0 of Spain250 500 1,000 San Jose CO Miles PA VEVE PA Panama GY GY © Copyright 2015 Willis Limited / Willis Re Inc. -
Hurricane Joaquin
HURRICANE TRACKING ADVISORY eVENT™ Hurricane Joaquin Information from NHC Advisory 14A, 8:00 AM EDT Thursday October 1, 2015 On the forecast track, the center of Joaquin will move near or over portions of the central Bahamas today and tonight and pass near or over portions of the northwestern Bahamas on Friday. Maximum sustained winds are near 120 mph with higher gusts. Joaquin is a category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale. Some strengthening is forecast in the next day or so, with some fluctuations in intensity possible on Friday. Intensity Measures Position & Heading U.S. Landfall (NHC) Max Sustained Wind 120 mph Position Relative to 10 miles N of Samana Cays Speed: (category 3) Land: Bahamas Est. Time & Region: n/a Min Central Pressure: 942 mb Coordinates: 23.2 N, 73.7 W Trop. Storm Force Est. Max Sustained Wind 140 miles Bearing/Speed: WSW or 240 degrees at 5 mph n/a Winds Extent: Speed: Forecast Summary Hurricane conditions are expected to continue in portions of the central and southeastern Bahamas through Friday. Hurricane conditions are expected over portions of the northwestern Bahamas on Friday. Tropical storm conditions will affect the southeastern Bahamas through tonight. A dangerous storm surge will raise water levels by as much as 5 to 8 feet above normal tide levels in the central Bahamas in areas of onshore flow. A storm surge of 2 to 4 feet above normal tide levels is expected in the northwest Bahamas within the hurricane warning area, and 1 to 2 feet is expected in the southeast Bahamas. -
Tropical Jets and Disturbances
Tropical Jets and Disturbances Introduction In previous lectures, we alluded to several types of disturbances found across the tropics, including the monsoon trough and intertropical convergence zone, that arise as a function or reflection of convergent flow across the tropics. Tropical cyclones, particularly in the western Pacific and Indian Oceans, commonly form out of one of these features. Before we proceed into the second half of the course and our studies on tropical cyclones, however, it is important for us to consider other types of tropical disturbances and jets that influence tropical cyclone activity. We also return to the concept of the tropical easterly jet, first introduced in our monsoons lecture, and further discuss its structure and impacts. Key Concepts • What is an African easterly wave? How do they form, grow, and decay? • What are the African and tropical easterly jets and how do they influence easterly waves and the meteorology of Africa? • What is the Saharan air layer and what are its characteristics? African Easterly Waves African easterly waves, or AEWs, are westward-travelling waves that originate over northern Africa primarily between June and October. They have approximate horizontal wavelengths of 2500 km, periods of 3-5 days, and move westward at a rate of 5-8 m s-1 (or 500-800 km per day). Previous theories for AEW formation suggested that they formed in response to the breakdown of the ITCZ or the growth of instabilities associated with the African easterly jet (AEJ). Current theory, however, suggests that AEWs form in response to latent heating associated with mesoscale convective systems that form along higher terrain in eastern Africa. -
Hurricane Joaquin
HURRICANE TRACKING ADVISORY eVENT™ Hurricane Joaquin Information from NHC Advisory 18A, 8:00 AM EDT Friday October 2, 2015 On the forecast track, the core of the strongest winds of Joaquin will continue moving over portions of the central and northwestern Bahamas today. Joaquin will begin to move away from the Bahamas tonight and Saturday. Maximum sustained winds are near 130 mph with higher gusts. Joaquin is a dangerous category 4 hurricane. Some fluctuations in intensity are possible during the next 24 hours. Slow weakening is expected to begin on Saturday. Intensity Measures Position & Heading U.S. Landfall (NHC) Max Sustained Wind 130 mph Position Relative to 30 miles NNE of Clarence Long Speed: (category 4) Land: Island Bahamas Est. Time & Region: n/a Min Central Pressure: 937 mb Coordinates: 23.4 N, 74.8 W Trop. Storm Force Est. Max Sustained Wind 205 miles Bearing/Speed: NW or 315 degrees at 3 mph n/a Winds Extent: Speed: Forecast Summary Hurricane conditions are expected to continue across portions of central and southeastern Bahamas through today. Hurricane and tropical storm conditions are expected over portions of the northwestern Bahamas today. Tropical storm conditions will affect other portions of the southeastern Bahamas, and the Turks and Caicos Islands today. Tropical storm conditions are expected over portions of eastern Cuba this morning. A dangerous storm surge will raise water levels by as much as 6 to 12 feet above normal tide levels in the central Bahamas in areas of onshore flow. A storm surge of 2 to 4 feet above normal tide levels is expected in the remainder of the Bahamas within the hurricane warning area. -
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. -
Regional Overview: Impact of Hurricanes Irma and Maria
REGIONAL OVERVIEW: IMPACT OF MISSION TO HURRICANES IRMA AND MARIA CONFERENCE SUPPORTING DOCUMENT 1 The report was prepared with support of ACAPS, OCHA and UNDP 2 CONTENTS SITUATION OVERVIEW ......................................................................................................................... 4 KEY FINDINGS ............................................................................................................................................ 5 Overall scope and scale of the impact ....................................................................................... 5 Worst affected sectors ...................................................................................................................... 5 Worst affected islands ....................................................................................................................... 6 Key priorities ......................................................................................................................................... 6 Challenges for Recovery ................................................................................................................. 7 Information Gaps ................................................................................................................................. 7 RECOMMENDATIONS FOR RECOVERY ................................................................................ 10 Infrastructure ...................................................................................................................................... -
African Easterly Jet in the ECMWF Integrated Forecast System: 4Dvar Analysis
453 African easterly jet in the ECMWF integrated forecast system: 4DVar analysis A. M. Tompkins1, A. Diongue2, D. J. Parker3 and C. D. Thorncroft4 Research Department 1 ECMWF 2 Direction de la Meteorologie Nationale, Dakar-Yoff, Senegal 3 Institute for Atmospheric Science, University of Leeds, Leeds, UK 4 Department of Earth and Atmospheric Science, University at Albany, New York, USA Submitted to Q.J. Roy. Meteor. Soc. December 2004 Series: ECMWF Technical Memoranda A full list of ECMWF Publications can be found on our web site under: http://www.ecmwf.int/publications/ Contact: [email protected] c Copyright 2004 European Centre for Medium-Range Weather Forecasts Shinfield Park, Reading, RG2 9AX, England Literary and scientific copyrights belong to ECMWF and are reserved in all countries. This publication is not to be reprinted or translated in whole or in part without the written permission of the Director. Appropriate non-commercial use will normally be granted under the condition that reference is made to ECMWF. The information within this publication is given in good faith and considered to be true, but ECMWF accepts no liability for error, omission and for loss or damage arising from its use. African easterly jet in 4DVar analysis Abstract In August 2000, the Met Office C130 research flight aircraft conducted four sorties over the Western Sahel region, making dropsonde measurements at an unprecedented resolution. These were used as an independent validation source to assess the quality of the analysis of the African easterly jet (AEJ) in the European Centre for medium range forecasts (ECMWF) integrated forecast system. -
Summary of 2002 Atlantic Tropical Cyclone Activity And
SUMMARY OF 2002 ATLANTIC TROPICAL CYCLONE ACTIVITY AND VERIFICATION OF AUTHORS' SEASONAL ACTIVITY FORECAST An Early Summer Successful Forecast of an Inactive Hurricane Season - But the Many Weak, Higher Latitude Tropical Storms That Formed Were Not Anticipated (as of 21 November 2002) By William M. Gray1, Christopher W. Landsea,2 and Philip Klotzbach3 with advice and assistance from William Thorson4 and Jason Connor5 [This verification as well as past forecasts and verifications are available via the World Wide Web: http://typhoon.atmos.colostate.edu/forecasts/] Brad Bohlander or Thomas Milligan, Colorado State University Media Representatives (970-491-6432) are available to answer questions about this verification. Department of Atmospheric Science Colorado State University Fort Collins, CO 80523 Phone Number: 970-491-8681 2002 ATLANTIC BASIN SEASONAL HURRICANE FORECAST Tropical Cyclone Parameters Updated Updated Updated Updated Observed and 1950-2000 Climatology 7 Dec 5 April 2002 31 May 2002 7 Aug 2002 2 Sep 2002 (in parentheses) 2001 Forecast Forecast Forecast Forecast Totals Named Storms (NS) (9.6) 13 12 11 9 8 12 Named Storm Days (NSD) (49.1) 70 65 55 35 25 54 Hurricanes (H)(5.9) 8 7 6 4 3 4 Hurricane Days (HD)(24.5) 35 30 25 12 10 11 Intense Hurricanes (IH) (2.3) 4 3 2 1 1 2 Intense Hurricane Days (IHD)(5.0) 7 6 5 2 2 2.5 Hurricane Destruction Potential (HDP) (72.7) 90 85 75 35 25 31 Net Tropical Cyclone Activity (NTC)(100%) 140 125 100 60 45 80 VERIFICATION OF 2002 MAJOR HURRICANE LANDFALL FORECAST 7 Dec 5 Apr 31 May 7 Aug Fcst. -
Preleminary Report IP and ETA&IOTA Hurricanes .Indd
PRELIMINARY REPORT November 2020 ConsequencesConsequences ofof thethe HurricaneHurricane 20202020 SeasonSeason onon IndigenousIndigenous CommunitiesCommunities inin CentralCentral AmericaAmerica Destruction and Resilience PRELIMINARY REPORT ON THE CONSEQUENCES OF THE 2020 HURRICANE SEASON ON INDIGENOUS COMMUNITIES IN CEN- TRAL AMERICA DESTRUCTION AND RESILIENCE NOVEMBER 2020 GENERAL COORDINATION Myrna Cunningham Kain - President of FILAC Board of Directors Jesús Amadeo Martínez - General Coordinator of the Indigenous Forum of AbyaYala FIAY GENERAL SUPERVISION Álvaro Pop - FILAC Technical Secretary Amparo Morales - FILAC Chief of Staff TECHNICAL TEAM Ricardo Changala - Coordinator of the Regional Observatory for the Rights of Indigenous Peoples ORDPI FILAC Liber- tad Pinto - Technical Team ORDPI-FILAC Jean Paul Guevara - Technical Team ORDPI-FILAC TECHNICAL SUPPORT Ernesto Marconi - FILAC Technical Program Management Gabriel Mariaca - Coordinator of Institutional Communication FILAC Dennis Mairena - Management of Technical Programs FILAC Wendy Medina - FILAC Communication and Press Office GRAPHIC DESIGN Institutional Communication - FILAC IMAGES FILAC Imaging Archive UN Photos Shutterstock Unsplash LICENSE FOR DISTRIBUTION CC-BY-NC 4.0 This license allows reusers to distribute, remix, adapt, and build upon the material in any medium or format for noncommercial purposes only, and only so long as attribution is given to the creator. Credit must be given to the creator Only noncommercial uses of the work are permitted DOGOTAL ACCESS ON: https://indigenascovid19.red/monitoreo/ FILAC 20 de Octubre 2287 esq. Rosendo Gutiérrez [email protected] La Paz, Bolivia SUPPORT Ford Foundation, AECID and Pawanka Fund Introduction This document is a preliminary report on the human and material impacts of hurricanes Eta and Iota on the Central American isthmus. It has been an extraordinary fact that two hurricanes of this size and strength have hit the region so close in time, affecting all Central American countries.