Conference Poster Production

Total Page:16

File Type:pdf, Size:1020Kb

Conference Poster Production 65th Interdepartmental Hurricane Conference Miami, Florida February 28 - March 3, 2011 Hurricane Earl:September 2, 2010 Ocean and Atmospheric Influences on Tropical Cyclone Predictions: Challenges and Recent Progress S E S S Session 2 I The 2010 Tropical Cyclone Season in Review O N 2 The 2010 Atlantic Hurricane Season: Extremely Active but no U.S. Hurricane Landfalls Eric Blake and John L. Beven II ([email protected]) NOAA/NWS/National Hurricane Center The 2010 Atlantic hurricane season was quite active, with 19 named storms, 12 of which became hurricanes and 5 of which reached major hurricane intensity. These totals are well above the long-term normals of about 11 named storms, 6 hurricanes, and 2 major hurricanes. Although the 2010 season was considerably busier than normal, no hurricanes struck the United States. This was the most active season on record in the Atlantic that did not have a U.S. landfalling hurricane, and was also the second year in a row without a hurricane striking the U.S. coastline. A persistent trough along the east coast of the United States steered many of the hurricanes out to sea, while ridging over the central United States kept any hurricanes over the western part of the Caribbean Sea and Gulf of Mexico farther south over Central America and Mexico. The most significant U.S. impacts occurred with Tropical Storm Hermine, which brought hurricane-force wind gusts to south Texas along with extremely heavy rain, six fatalities, and about $240 million dollars of damage. Hurricane Earl was responsible for four deaths along the east coast of the United States due to very large swells, although the center of the hurricane stayed offshore. Session 2 – Page 1 Overview of the 2010 Eastern North Pacific Hurricane Season John P. Cangialosi and Stacy R. Stewart ([email protected] and [email protected] ) NOAA/NWS Tropical Prediction Center/National Hurricane Center The 2010 eastern North Pacific hurricane season was historically the least active on record. Only seven tropical storms developed, three of which became hurricanes. This is the lowest number of tropical storms and hurricanes observed since routine satellite reconnaissance of the basin began in 1971. Five tropical depressions formed this season that did not strengthen into tropical storms. The Accumulated Cyclone Energy (ACE) index for 2010 was 46% of the long-term median. This is the third lowest ACE value, ahead of only the 2007 and 1997 seasons. Although the season was inactive, Tropical Storm Agatha was a high impact event causing 160 deaths and significant damage to portions of Central America and Mexico. This, along with other season highlights will be presented. In addition, some of the operational challenges encountered during the season will also be discussed. Session 2 – Page 2 2010 Atlantic and Eastern North Pacific Forecast Verification James L. Franklin ([email protected]) NOAA/NWS/National Hurricane Center A verification of official track, intensity, and genesis forecasts from the National Hurricane Center during the 2010 season will be presented, along with a discussion of the performance of the guidance models. Session 2 – Page 3 Review of the 2010 Central Pacific Tropical Cyclone Season and Preliminary Verification Raymond Tanabe ([email protected]) Deputy Director, Central Pacific Hurricane Center (CPHC) In 2010, there was one tropical cyclone to have formed in or moved into the central Pacific. Tropical Storm Omeka originated as a subtropical storm west of the dateline and transitioned into a tropical cyclone just east of the dateline on 20 December 2010. CPHC will present an overview of Tropical Storm Omeka, the preliminary verification, changes for the 2011 season, and recent staff changes. Session 2 – Page 4 A Review of the Joint Typhoon Warning Center 2010 Tropical Cyclone Season Mr. Robert J. Falvey ([email protected]) Joint Typhoon Warning Center A review of the 2010 tropical cyclone activity with discussion of significant events for the JTWC Pacific and Indian Ocean forecast areas of responsibility will be presented. Session 2 – Page 5 53d Weather Reconnaissance Review of the 2010 Hurricane Season Capt Douglas Gautrau ([email protected]) 53d Weather Reconnaissance Squadron The 2010 hurricane season was a slightly below average year for the 53d Weather Reconnaissance Squadron with 981.4 total flying hours (compared to 1062 average flying hours per season over the previous 10 years). Although the storm season seemed relatively slow due to the lack of storms in the Gulf of Mexico, we stayed very busy flying the majority of our flights in the Caribbean Sea and Atlantic Ocean. We flew a total of 100 tasked missions meeting 97% of our requirements. Overall, the Stepped Frequency Microwave Radiometer once again performed reasonably well on ten WC-130J aircraft, providing critical surface wind speed and rainfall rate data to the customer. Operator experience increased with the instrument and valuable inputs and improvements to instrument performance were accomplished. Session 2 – Page 6 NOAA Aircraft Operations Center (AOC) 2010 Seasonal Summary and Future Plans Jim McFadden, Nancy Ash, Jack Parrish, Paul Flaherty, A. Barry Damiano, Ian Sears, Jessica Williams, Richard Henning ([email protected]) NOAA Aircraft Operations Center After a relatively slow season in 2009, during which NOAA aircraft flew a total of 62 flights and 326 hrs, the 2010 season was a bit more active with its three hurricane aircraft, two WP-3Ds and the Gulfstream G-IV, flying 71 flights for 453 hours. These flights, in addition to storm flights, included trips for public awareness, such as the Gulf Coast Hurricane Awareness Tour and the Governor’s Hurricane Conference, test and calibration flights as well as several transit flights. Of significance during the 2010 season was the joint NASA, NOAA and NSF operation that utilized a number of aircraft from each of the Agencies in a study of tropical storm genesis and rapid intensification. In addition to NOAA’s three aircraft, NASA provided its DC-8, aWB-57 and Global Hawk. The NSF provided the Gulfstream G-V. These aircraft often flew coordinated patterns associated with tropical systems in the Atlantic and Caribbean. The three NOAA aircraft also obtained the most comprehensive data set on the development and decay of a tropical system when they flew Hurricane Earl practically from the cradle to the grave – from genesis to extra-tropical transition. AOC continues to upgrade its aircraft and instrumentation, and in 2011 expects to accomplish the following: • Complete the acceptance tests of the tail Doppler radar on the NOAA G-IV • Continue developing strategies for use of the new G-IV TDR in storm environment • Complete the avionics upgrade on N44RF, NOAA’s 3rd P-3 • Complete integration of new aircraft data system (AAMPS) on the NOAA P-3s • Complete installation of new AXBT receivers on both P-3s Session 2 – Page 7 S E S Session 3 S Observations and I Observing Strategies for Tropical Cyclones and O their Environment, Part 1 N 3 Microwave sounder observations during GRIP: Preliminary results Bjorn Lambrigtsen, Shannon Brown ([email protected]) Jet Propulsion Laboratory, California Institute of Technology The High Altitude MMIC Sounding Radiometer (HAMSR), a microwave sounder similar to but more advanced than the AMSU sounders now operating on multiple satellites, was deployed on the Global Hawk unmanned aircraft during the Genesis and Rapid Intensification Processes (GRIP) hurricane field campaign during August and September 2010. HAMSR was developed at the Jet Propulsion Laboratory more than ten years ago and has been flown in several hurricane field campaigns. It was recently upgraded with the latest technology and is now the most sensitive and accurate sensor of its kind. Using observations from previous field campaigns, a new algorithm has been developed that makes it possible to emulate a radar and derive reflectivity profiles from the observed brightness temperatures. We present preliminary results from GRIP, including close-up views of the convective structure of Hurricane Karl as it intensified to category 3. The Global Hawk flew over Karl for 13 hours and passed over the eye 20 times during this period, and with HAMSR it is possible to analyze the three-dimensional convective structure of the inner core as it evolves. And since HAMSR is a sounder, it is also possible to analyze the thermodynamic structure in areas surrounding the core. GRIP was operated in coordination with NOAA and the NSF, and observations were collected from numerous sensors on multiple aircraft platforms. The analysis of this rich data set is just beginning. Copyright 2011 California Institute of Technology. Government sponsorship acknowledged. Session 3 – Page 1 NPP Microwave-sounder Based Tropical Cyclone Products Andrea Schumacher1, Mark DeMaria2, John A. Knaff2, Limin Zhao3, Tom Schott4 ([email protected]) 1Cooperative Institute for Research in the Atmosphere, Fort Collins, CO; 2NOAA/NESDIS/STAR, Fort Collins, CO; 3NOAA/NESDIS/OSPO/SPSD, Camp Springs, MD; 4NOAA/NESDIS/OSD, Suitland, MD NESDIS provides several Advanced Microwave Sounding Unit (AMSU)-based operational tropical cyclone (TC) intensity and structure guidance products. Using temperature retrievals corrected for scattering and attenuation a number of tropical cyclone products are generated. These products include storm-centered radius vs. pressure profiles of temperature and gradient winds, objective estimates of 1-min maximum sustained surface winds, minimum sea level pressure, the radii of 34-, 50-, and 64-kt winds in the northeast, southeast, southwest, and northwest quadrants, and balanced horizontal winds on standard pressure levels from 1000 hPa to 100 hPa within 600 km of tropical cyclones. Product algorithms use statistical methods to remove temperature biases due to scattering and attenuation, and by using NCEP boundary conditions and hydrostatic balance heights fields can be estimated.
Recommended publications
  • Temporary Protected Status for Guatemalans
    Guatemala Human Rights Commission / USA Fact Sheet Temporary Protected Status for Guatemalans Guatemalans are in urgent need of TPS due to the recent natural disasters in their home country. The economic and environmental damage has been devastating and Guatemalans living and working in the U.S. should not be forced to return to a disaster-stricken area. Additionally, families depend on financial support from their relatives in the U.S.; TPS would support the continued reconstruction of the devastation caused by tropical storms, intense rains, and volcanic activity. What is TPS? Temporary Protected Status (TPS) is a benefit granted by the Department of Homeland Security (DHS) that permits individuals from selected countries to remain in the United States for a certain amount of time, regardless of previous immigration status. Grants of TPS are initially made for periods of 6 to 18 months and may be extended depending on the situation. Removal proceedings are suspended for those granted TPS. DHS may grant TPS to countries due to: If granted TPS, individuals: Ongoing armed conflicts (such as civil wars) Cannot be removed from the U.S. Environmental disasters (such as hurricanes or Cannot be detained by DHS earthquakes) Can obtain an employment authorization document Other extraordinary or temporary conditions Are eligible for travel authorization TPS does not lead to permanent resident status. After the designated time period has expired, previous immigration status is restored. Pacaya Eruption and Tropical Storms On May 27, 2010, the Pacaya Volcano erupted just south of Guatemala City, forcing 2,000 people to evacuate. This was only the beginning.
    [Show full text]
  • Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific Ab Sins Nicholas S
    Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School March 2019 Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific aB sins Nicholas S. Grondin Louisiana State University, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Climate Commons, Meteorology Commons, and the Physical and Environmental Geography Commons Recommended Citation Grondin, Nicholas S., "Climatology, Variability, and Return Periods of Tropical Cyclone Strikes in the Northeastern and Central Pacific asinB s" (2019). LSU Master's Theses. 4864. https://digitalcommons.lsu.edu/gradschool_theses/4864 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. CLIMATOLOGY, VARIABILITY, AND RETURN PERIODS OF TROPICAL CYCLONE STRIKES IN THE NORTHEASTERN AND CENTRAL PACIFIC BASINS A Thesis Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Master of Science in The Department of Geography and Anthropology by Nicholas S. Grondin B.S. Meteorology, University of South Alabama, 2016 May 2019 Dedication This thesis is dedicated to my family, especially mom, Mim and Pop, for their love and encouragement every step of the way. This thesis is dedicated to my friends and fraternity brothers, especially Dillon, Sarah, Clay, and Courtney, for their friendship and support. This thesis is dedicated to all of my teachers and college professors, especially Mrs.
    [Show full text]
  • Hurricane and Tropical Storm
    State of New Jersey 2014 Hazard Mitigation Plan Section 5. Risk Assessment 5.8 Hurricane and Tropical Storm 2014 Plan Update Changes The 2014 Plan Update includes tropical storms, hurricanes and storm surge in this hazard profile. In the 2011 HMP, storm surge was included in the flood hazard. The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, severity, warning time and secondary impacts. New and updated data and figures from ONJSC are incorporated. New and updated figures from other federal and state agencies are incorporated. Potential change in climate and its impacts on the flood hazard are discussed. The vulnerability assessment now directly follows the hazard profile. An exposure analysis of the population, general building stock, State-owned and leased buildings, critical facilities and infrastructure was conducted using best available SLOSH and storm surge data. Environmental impacts is a new subsection. 5.8.1 Profile 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 (National Oceanic and Atmospheric Administration [NOAA] 2013a). 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.
    [Show full text]
  • TROPICAL STORM AMANDA (EP022020) 30–31 May 2020
    NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT TROPICAL STORM AMANDA (EP022020) 30–31 May 2020 Robbie Berg National Hurricane Center 10 September 2020 GOES-EAST GEOCOLOR IMAGE OF TROPICAL STORM AMANDA AT 1200 UTC 31 MAY 2020, A COUPLE OF HOURS AFTER THE STORM MADE LANDFALL IN SOUTHEASTERN GUATEMALA (IMAGE COURTESY OF NOAA/NESDIS/STAR) Amanda is the second-known tropical storm to make landfall along the Pacific coast of Guatemala, after Tropical Storm Agatha of 2010. In conjunction with a larger weather system over Central America and Tropical Storm Cristobal over the Bay of Campeche, Amanda produced significant rainfall and flooding over portions of Central America and southeastern Mexico, resulting in 40 deaths in El Salvador, Guatemala, and Honduras. Tropical Storm Amanda 2 Tropical Storm Amanda 30–31 MAY 2020 SYNOPTIC HISTORY Multiple factors appear to have led to Amanda’s formation. The convectively active phase of an eastward-moving Kelvin wave spread over the far eastern part of the North Pacific Ocean between 26 and 31 May, while at the same time a mid- to upper-level low closed off over northeastern Mexico. The upper-level diffluence associated with these features caused an overall increase in convection over the far eastern Pacific during that period, as well as the development of a broad area of low pressure south of Guatemala and El Salvador by 27 May. A low-latitude tropical wave, which had moved off the coast of Africa around 18 to 19 May, moved into the Pacific basin on 29 May and caused the broad low and associated convection to become more organized.
    [Show full text]
  • State of the Climate in 2016
    STATE OF THE CLIMATE IN 2016 Special Supplement to the Bullei of the Aerica Meteorological Society Vol. 98, No. 8, August 2017 STATE OF THE CLIMATE IN 2016 Editors Jessica Blunden Derek S. Arndt Chapter Editors Howard J. Diamond Jeremy T. Mathis Ahira Sánchez-Lugo Robert J. H. Dunn Ademe Mekonnen Ted A. Scambos Nadine Gobron James A. Renwick Carl J. Schreck III Dale F. Hurst Jacqueline A. Richter-Menge Sharon Stammerjohn Gregory C. Johnson Kate M. Willett Technical Editor Mara Sprain AMERICAN METEOROLOGICAL SOCIETY COVER CREDITS: FRONT/BACK: Courtesy of Reuters/Mike Hutchings Malawian subsistence farmer Rozaria Hamiton plants sweet potatoes near the capital Lilongwe, Malawi, 1 February 2016. Late rains in Malawi threaten the staple maize crop and have pushed prices to record highs. About 14 million people face hunger in Southern Africa because of a drought that has been exacerbated by an El Niño weather pattern, according to the United Nations World Food Programme. A supplement to this report is available online (10.1175/2017BAMSStateoftheClimate.2) How to cite this document: Citing the complete report: Blunden, J., and D. S. Arndt, Eds., 2017: State of the Climate in 2016. Bull. Amer. Meteor. Soc., 98 (8), Si–S277, doi:10.1175/2017BAMSStateoftheClimate.1. Citing a chapter (example): Diamond, H. J., and C. J. Schreck III, Eds., 2017: The Tropics [in “State of the Climate in 2016”]. Bull. Amer. Meteor. Soc., 98 (8), S93–S128, doi:10.1175/2017BAMSStateoftheClimate.1. Citing a section (example): Bell, G., M. L’Heureux, and M. S. Halpert, 2017: ENSO and the tropical Paciic [in “State of the Climate in 2016”].
    [Show full text]
  • 1858 San Diego Hurricane and Not Be Sur- Documented to Be Real
    THE SAN DIEGO HURRICANE OF 2 OCTOBER 1858 BY MICHAEL CHENOWETH AND CHRISTOPHER LANDSEA The discovery of a hurricane that directly impacted San Diego, California, nearly 150 yr ago has implications for residents and risk managers in their planning for extreme events for the region. ropical cyclones forming in the eastern North 10 September 1976 in California and Arizona, and Pacific Ocean are occasional visitors to the Hurricane Nora in September 1997 in Arizona. Only T southwestern United States. By the time these the 1939 tropical storm made a direct landfall in coastal systems travel far enough to the north to bring their California (Smith 1986), because the other three sys- associated moisture to the United States, the tropical tems entered the United States after first making land- cyclones have normally diminished below tropical fall in Mexico. storm strength over Mexico or over the colder waters The 1939 tropical storm caused $2 million in prop- of the California Current that flows southward along erty damage in California, mostly to shipping, shore the California coast. Rain, sometimes locally excessive, structures, power and communication lines, and crops. is frequently observed in many areas of the southwest- Ships in coastal waters of southern California reported ern United States when tropical cyclone remnants en- southeast winds between 34 and 47 kt (Hurd 1939). ter the region (Blake 1935; Smith 1986). However, no tropical cyclones are recorded or esti- Four tropical cyclones have managed to bring tropi- mated to have made landfall in the southwestern cal storm–force winds to the southwestern United United States as a hurricane, with maximum 1-min States during the twentieth century: a tropical storm surface (10 m) winds of at least 64 kt.
    [Show full text]
  • 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.
    [Show full text]
  • 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 $100 billion in damages in the United States alone, making 2005 the costliest hurricane season of record. 1. Introduction intervals for all tropical and subtropical cyclones with intensities of 34 kt or greater; Bell et al. 2000), the 2005 By almost all standards of measure, the 2005 Atlantic season had a record value of about 256% of the long- hurricane season was the most active of record.
    [Show full text]
  • World Bank Document
    Document of The World Bank Report No: ICR2286 Public Disclosure Authorized IMPLEMENTATION COMPLETION AND RESULTS REPORT (IBRD-72380 IDA-39360 IDA-44980) ON A LOAN Public Disclosure Authorized IN THE AMOUNT OF US$ 3.7 MILLION AND ON CREDITS (2) IN THE AMOUNT OF SDR 2.6 MILLION (US$ 3.8 MILLION EQUIVALENT) SDR 1.9 MILLION (US$ 3 MILLION EQUIVALENT) Public Disclosure Authorized TO SAINT LUCIA FOR A DISASTER MANAGEMENT PROJECT II August 29, 2012 Sustainable Development Department Caribbean Country Management Unit Public Disclosure Authorized Latin America and the Caribbean Region CURRENCY EQUIVALENTS (Exchange Rate Effective June 2012) Currency Unit = Eastern Caribbean Dollars (EC$) US$ 1.00 = EC$ 2.70 FISCAL YEAR January 1 to December 31 ABBREVIATIONS AND ACRONYMS APL Adaptable Program Loan CAS Country Assistance Strategy CDERA Caribbean Disaster Emergency Response Agency CDEMA Caribbean Disaster and Emergency Management Agency CDMP Caribbean Disaster Mitigation Project DMP II Disaster Management Project II ECCB Eastern Caribbean Central Bank EIA Environmental Impact Assessment EOC Emergency Operations Center ERDMP Emergency Recovery and Disaster Management Project ERP Emergency Recovery Project EU European Union IBRD International Bank for Reconstruction and Development IDA International Development Association IADB Inter-American Development Bank LAC Latin America and the Caribbean MCWT&PU Ministry of Communications, Works, Transport and Public Utilities MOE Ministry of Education MOH Ministry of Health MPDE&H Ministry of Physical Development,
    [Show full text]
  • AMS Journals: Unsurpassed Quality, a Lasting Legacy, and Competitive Speed to Publication
    LETTER FROM HEADQUARTERS AMS Journals: Unsurpassed Quality, a Lasting Legacy, and Competitive Speed to Publication hile AMS journals have always maintained a that takes the manuscript through editing, typesetting, level of quality that was unsurpassed in the and layout into final form as a high-quality archived W atmospheric and related sciences—by virtu- article in both full-function XML and PDF (plus print ally any measure you might care to focus on—there for those who still receive the journals in this format) was a period when they were less competitive is also occurring in record time—currently on the than some journals in our field when it came to the order of 60 days and improving continually. The level speed of publication. of editorial and produc- As many authors have tion work carried out happily learned in re- on manuscripts ensures cent years, this has not that the resulting article been the reality with is one that authors can AMS journals for some be proud of and one time—but the impres- that reflects well on sion still lingers in some the author when ac- quarters. So forgive cessed by scholars in me if you’ve heard this the future. before, but the steady The AMS journals improvements over re- have a long reputation cent years in the time of publishing seminal to first reviews means works, and the AMS that all the journals imprimatur is synony- making up the AMS mous with quality. AMS suite are now boasting review times in the range of authors do not need to make a choice between speed 50 days on average.
    [Show full text]
  • Mariner's Guide for Hurricane Awareness
    Mariner’s Guide For Hurricane Awareness In The North Atlantic Basin Eric J. Holweg [email protected] Meteorologist Tropical Analysis and Forecast Branch Tropical Prediction Center National Weather Service National Oceanic and Atmospheric Administration August 2000 Internet Sites with Weather and Communications Information Of Interest To The Mariner NOAA home page: http://www.noaa.gov NWS home page: http://www.nws.noaa.gov NWS marine dissemination page: http://www.nws.noaa.gov/om/marine/home.htm NWS marine text products: http://www.nws.noaa.gov/om/marine/forecast.htm NWS radio facsmile/marine charts: http://weather.noaa.gov/fax/marine.shtml NWS publications: http://www.nws.noaa.gov/om/nwspub.htm NOAA Data Buoy Center: http://www.ndbc.noaa.gov NOAA Weather Radio: http://www.nws.noaa.gov/nwr National Ocean Service (NOS): http://co-ops.nos.noaa.gov/ NOS Tide data: http://tidesonline.nos.noaa.gov/ USCG Navigation Center: http://www.navcen.uscg.mil Tropical Prediction Center: http://www.nhc.noaa.gov/ High Seas Forecasts and Charts: http://www.nhc.noaa.gov/forecast.html Marine Prediction Center: http://www.mpc.ncep.noaa.gov SST & Gulfstream: http://www4.nlmoc.navy.mil/data/oceans/gulfstream.html Hurricane Preparedness & Tracks: http://www.fema.gov/fema/trop.htm Time Zone Conversions: http://tycho.usno.navy.mil/zones.html Table of Contents Introduction and Purpose ................................................................................................................... 1 Disclaimer ...........................................................................................................................................
    [Show full text]
  • National Weather Service Reference Guide
    National Weather Service Reference Guide Purpose of this Document he National Weather Service (NWS) provides many products and services which can be T used by other governmental agencies, Tribal Nations, the private sector, the public and the global community. The data and services provided by the NWS are designed to fulfill us- ers’ needs and provide valuable information in the areas of weather, hydrology and climate. In addition, the NWS has numerous partnerships with private and other government entities. These partnerships help facilitate the mission of the NWS, which is to protect life and prop- erty and enhance the national economy. This document is intended to serve as a reference guide and information manual of the products and services provided by the NWS on a na- tional basis. Editor’s note: Throughout this document, the term ―county‖ will be used to represent counties, parishes, and boroughs. Similarly, ―county warning area‖ will be used to represent the area of responsibility of all of- fices. The local forecast office at Buffalo, New York, January, 1899. The local National Weather Service Office in Tallahassee, FL, present day. 2 Table of Contents Click on description to go directly to the page. 1. What is the National Weather Service?…………………….………………………. 5 Mission Statement 6 Organizational Structure 7 County Warning Areas 8 Weather Forecast Office Staff 10 River Forecast Center Staff 13 NWS Directive System 14 2. Non-Routine Products and Services (watch/warning/advisory descriptions)..…….. 15 Convective Weather 16 Tropical Weather 17 Winter Weather 18 Hydrology 19 Coastal Flood 20 Marine Weather 21 Non-Precipitation 23 Fire Weather 24 Other 25 Statements 25 Other Non-Routine Products 26 Extreme Weather Wording 27 Verification and Performance Goals 28 Impact-Based Decision Support Services 30 Requesting a Spot Fire Weather Forecast 33 Hazardous Materials Emergency Support 34 Interactive Warning Team 37 HazCollect 38 Damage Surveys 40 Storm Data 44 Information Requests 46 3.
    [Show full text]