A Report on All Cyclones That Formed in 2017, with Detailed Season Statistics and Records That Were Achieved Worldwide This Year
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HURRICANE KENNETH (EP132017) 18–23 August 2017
NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT HURRICANE KENNETH (EP132017) 18–23 August 2017 Robbie Berg National Hurricane Center 26 January 2018 NASA-NOAA SUOMI NPP ENHANCED INFRARED SATELLITE IMAGE OF HURRICANE KENNETH AT 1034 UTC 21 AUGUST 2017 WHILE AT PEAK INTENSITY Kenneth was a category 4 hurricane (on the Saffir-Simpson Hurricane Wind Scale) over the eastern North Pacific Ocean that did not affect land. Hurricane Kenneth 2 Hurricane Kenneth 18–23 AUGUST 2017 SYNOPTIC HISTORY Kenneth formed from the interaction of two tropical waves which moved off the west coast of Africa on 29 July and 2 August. The first wave moved across the Atlantic Ocean and northern South America at low latitudes and reached the eastern North Pacific Ocean on 8 August. At that point, the wave became more convectively active, but it moved only slowly westward for the next week due to its position south of Hurricane Franklin over the Bay of Campeche. In the meantime, the second tropical wave spawned Hurricane Gert over the western Atlantic, with the southern portion of the wave reaching the eastern North Pacific waters on 12 August. With the subtropical ridge rebuilding over the Gulf of Mexico, the second wave moved at a faster speed toward the west and reached the first tropical wave on 16 August (Fig. 1). The interaction of the two waves caused the development of a low by 1200 UTC 17 August about 530 n mi southwest of Manzanillo, Mexico. Convective banding became more organized and persistent through the day, and the low was designated as a tropical depression by 0600 UTC 18 August about 585 n mi south- southwest of the southern tip of the Baja California peninsula. -
Cyclone Enawo MADAGASCAR
Madagascar: Cyclone Enawo Situation Report No. 2 12 March 2017 This report is issued by the Bureau National de Gestion des Risques et des Catastrophes (BNGRC) and the Humanitarian Country Team in Madagascar. It covers the period from 9 to 12 March. The next report will be issued on or around 14 March 2017. Highlights • The remnants of Intense Tropical Cyclone Enawo exited Madagascar on the morning of Friday 10 March 2017. The storm traversed nearly the length of the island over two days, affecting communities from north to south across Madagascar’s eastern and central regions. • Wind damage and widespread flooding in cyclone- affected parts of the north-east, and heavy rains and widespread flooding in eastern, central and south- eastern parts of the country has been recorded. • Favourable weather conditions since 10 March have permitted national authorities and humanitarian partners to initiate rapid assessments in north- eastern, eastern and south-eastern parts of the country. • Initial humanitarian impacts in the areas of Water, Sanitation and Hygiene (WASH), Shelter, Health, Food Security, Protection and Education, as well as Logistics have been identified. • Field coordination hubs are being jointly reinforced by national authorities and humanitarian partners in Maroantsetra and Antalaha. 295,950 84,660 83,100 58 Affected people Displaced people Damaged houses Affected districts Source: Bureau National de Gestion des Risques et des Catastrophes (BNGRC) de Madagascar, 12 March 2017 Situation Overview Intense Tropical Cyclone Enawo made landfall in north-eastern Madagascar’s Sava region on 7 March and then moved southward in an arc across central and south-eastern parts of the country as a tropical depression before exiting the country on the morning of 10 March. -
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. -
Madagascar Enawo Report En.Pdf
Preparedness and response to cyclones From the Prime Minister Head of Government, and floods in Madagascar, a concrete Minister of Interior and Decentralization progress Madagascar is the most exposed country to cyclone in Africa and the third most vulnerable to climate change in the World. An annual average of his report is based on the passage of 1 to 2 cyclones directly strike the country, causing immediate and long-term Intense Tropical Cyclone Enawo which direct consequences. They weaken both the affected households and the Taffected Madagascar in March 2017, economy of the country. The economic losses caused by a strong cyclone the strongest cyclone experienced by the are typically around 4% of the national Gross Domestic Product. country over the last 10 years. Fully aware of this real and permanent threat, the Malagasy Government, with the support of all partners, has yclone Enawo came in through the reinforced its efforts to strengthen resilience, reduce risks and prepare for disasters in Madagascar. Between North East of the country, at the level of 2015 and 2017, approximately $US 30 million were invested in this area which targeted the most vulnerable CAntalaha district, as a strong category regions to natural disasters. These efforts have obviously started to bear fruit if we refer to the results achieved 4 cyclone on Monday 06 March 2017 at night. Enawo then swept through the country striking when Intense Tropical Cyclone Enawo struck in March 2017. The resilience capacity of the community allowed to the highlands and got out of the country on limit damages and losses incurred by the passage of this cyclone. -
4. the TROPICS—HJ Diamond and CJ Schreck, Eds
4. THE TROPICS—H. J. Diamond and C. J. Schreck, Eds. Pacific, South Indian, and Australian basins were a. Overview—H. J. Diamond and C. J. Schreck all particularly quiet, each having about half their The Tropics in 2017 were dominated by neutral median ACE. El Niño–Southern Oscillation (ENSO) condi- Three tropical cyclones (TCs) reached the Saffir– tions during most of the year, with the onset of Simpson scale category 5 intensity level—two in the La Niña conditions occurring during boreal autumn. North Atlantic and one in the western North Pacific Although the year began ENSO-neutral, it initially basins. This number was less than half of the eight featured cooler-than-average sea surface tempera- category 5 storms recorded in 2015 (Diamond and tures (SSTs) in the central and east-central equatorial Schreck 2016), and was one fewer than the four re- Pacific, along with lingering La Niña impacts in the corded in 2016 (Diamond and Schreck 2017). atmospheric circulation. These conditions followed The editors of this chapter would like to insert two the abrupt end of a weak and short-lived La Niña personal notes recognizing the passing of two giants during 2016, which lasted from the July–September in the field of tropical meteorology. season until late December. Charles J. Neumann passed away on 14 November Equatorial Pacific SST anomalies warmed con- 2017, at the age of 92. Upon graduation from MIT siderably during the first several months of 2017 in 1946, Charlie volunteered as a weather officer in and by late boreal spring and early summer, the the Navy’s first airborne typhoon reconnaissance anomalies were just shy of reaching El Niño thresh- unit in the Pacific. -
Baseline Assessment Study on Wastewater Management Belize
Caribbean Regional Fund for Wastewater Management Baseline Assessment Study on Wastewater Management Belize December 2013 Revised January 2015 Baseline Assessment Study for the GEF CReW Project: Belize December 2013 Prepared by Dr. Homero Silva Revised January 2015 CONTENTS List of Acronyms....................................................................................................................................................iii 1. Introduction ........................................................................................................................................................ 1 2. The National Context ....................................................................................................................................... 3 Description of the Country .................................................................................................................. 4 Geographic Characteristics ................................................................................................................. 6 Economy by Sectors ............................................................................................................................ 9 The Environment .............................................................................................................................. 13 Land Use, Land Use Changes and Forestry (LULUCF) ....................................................................... 20 Disasters .......................................................................................................................................... -
National Climate Change Risk Assessment for New Zealand: Technical Report
National Climate Change Risk Assessment for New Zealand Arotakenga Tūraru mō te Huringa Āhuarangi o Āotearoa Technical report Pūrongo Whaihanga This document may be cited as: Ministry for the Environment. 2020. National Climate Change Risk Assessment for New Zealand – Arotakenga Tūraru mō te Huringa Āhuarangi o Āotearoa: Technical report – Pūrongo whaihanga. Wellington: Ministry for the Environment. Disclaimer The information in this publication is, according to the Ministry for the Environment’s best efforts, accurate at the time of publication. The information provided does not alter the laws of New Zealand and other official guidelines or requirements. Users should take specific advice from qualified professional people before undertaking any action, as a result of information obtained from this publication. The Ministry for the Environment does not accept any responsibility or liability whether in contract, tort, equity or otherwise, for any action taken as a result of reading, or reliance placed on the Ministry for the Environment because of having read any part, or all, of the information in this publication or for any error, or inadequacy, deficiency, flaw in or omission from the information provided in this publication. Acknowledgements Prepared for the Ministry for the Environment by a consortium led by AECOM, including Tonkin + Taylor Ltd, NIWA and Latitude and a number of independent contractors. Published in July 2020 by the Ministry for the Environment Manatū Mō Te Taiao PO Box 10362, Wellington 6143, New Zealand ISBN: 978-1-98-857995-5 (online) Publication number: ME 1508 © Crown copyright New Zealand 2020 This document is available on the Ministry for the Environment website: www.mfe.govt.nz. -
Unique Aspects of the Vanilla Market MARKET + OUTLOOK MARKET + OUTLOOK
MARKET MARKET OUTLOOK OUTLOOK Unique Aspects of the Vanilla Market MARKET + OUTLOOK MARKET + OUTLOOK + Daniel Aviles Commodity Information Analyst McKeany-Flavell Commodities. Ingredients. Intelligence. McKeany-Flavell © 2018 McKeany-Flavell Company, Inc. All rights reserved. Commodities. Ingredients. Intelligence. Distribution is prohibited without written permission from McKeany-Flavell. McKeany-Flavell Unique Aspects of the Vanilla Market Commodities. Ingredients. Intelligence. Unique Aspects of the Vanilla Market “Money is the best fertilizer” and “the cure for high prices is high prices” may sound like commodity clichés, but they are not mere truisms. Every market will eventually return to these rules, a lesson we advise our clients to remember. Yet there is always an exception: For vanilla, it often seems that the rules are reversed, and price shifts have counterintuitive effects. This ingredient is a challenge for all players, from growers through processors to end users, but understanding vanilla’s supply cycle and pricing dynamics may at least partially demystify this market. What sets the vanilla market apart: + Difficulty: Cultivation is extremely labor Vanilla fruit, pod, or bean with closeup of seeds intensive, and a high degree of expertise is needed to grow the plants and process the pods (beans). + Vulnerability: Production is significantly What Is Vanilla? concentrated in one origin, Madagascar, which has in the past crowded out A quick introduction: Vanilla is a flavor made from the pod-like competing origins. The natural food trend fruit of some members of the vanilla genus of the orchid family, has now made demand less elastic, and pricing may follow suit. the only orchid that yields an edible fruit commercially cultivated for food use; vanilla fruit is widely referred to as a “bean,” a + Price pressures: Early harvest is commercially viable and is encouraged convention that we follow here. -
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. -
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. -
A Year in Review 2016-2017 Women Leading Through Philanthropy CONTENTS It’S What’S on the Inside That Counts a Year in Review 2016-2017
a year in review 2016-2017 women leading through philanthropy CONTENTS it’s what’s on the inside that counts a year in review 2016-2017 Thank you from Society of Women Leaders CONTENTS Interim Co-Chairs Anita Pahor and Susan Wynne 4 it’s what’s on the A message of support from Australian Red Cross CEO Judy Slatyer 6 inside that counts Our vision 7 Transforming lives: the impact of our philanthropy 8 Young Parents Program 9 International Aid Workers 11 Migration Support Programs 14 Empowering communities in Indonesia 16 A daily phone call for people living alone 18 A year of action: philanthropy, education and friendship 20 Our members, very special gentlemen and supporters 23 Strategy, planning and leadership 24 About Red Cross 26 Inside cover image: Australian Red Cross deployed Aid Worker Jess Lees as part of a Field Assessment and Coordination Team to Somaliland. 3 Anita Pahor & Susan Wynne Co-Chairs Society of Women Leaders thank It has been our privilege to lead this remarkable circle of giving during the YOU past few months, together with Interim Partnership Advisers Rowena McGilvray and Kate O’Callaghan. One of the privileges and responsibilities of being a member of this circle of giving is becoming more educated about humanitarian issues that face our communities. We gain access to the world’s best minds and most active agents of humanitarian diplomacy. Australian Red Cross CEO Judy Slatyer and her senior staff personally share their vision for the organisation with us and discuss their plans to mobilise even more people in the Australian community to commit to humanitarian values. -
Rockhampton's Resilient Future
ROCKHAMPTON’S RESILIENT FUTURE DESIGN CHARRETTE Centre for Subtropical Design Queensland University of Technology 2 George Street GPO Box 2434 Brisbane QLD 4001 Australia Rosemary Kennedy Liz Brogden December 2015 Page 1 of 45 TABLE OF CONTENTS Executive Summary ..................................................................................................................................................................5 Introduction ..................................................................................................................................................................................6 Background ...................................................................................................................................................................................7 Rockhampton ..........................................................................................................................................................................7 Impact ....................................................................................................................................................................................8 The South Rockhampton Flood Levee Proposal .............................................................................................. 9 Objectives .................................................................................................................................................................................... 10 Approach and Methodology .............................................................................................................................................