Hitting Home: the Compounding Costs of Climate Inaction
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Cruising Guide to the Philippines
Cruising Guide to the Philippines For Yachtsmen By Conant M. Webb Draft of 06/16/09 Webb - Cruising Guide to the Phillippines Page 2 INTRODUCTION The Philippines is the second largest archipelago in the world after Indonesia, with around 7,000 islands. Relatively few yachts cruise here, but there seem to be more every year. In most areas it is still rare to run across another yacht. There are pristine coral reefs, turquoise bays and snug anchorages, as well as more metropolitan delights. The Filipino people are very friendly and sometimes embarrassingly hospitable. Their culture is a unique mixture of indigenous, Spanish, Asian and American. Philippine charts are inexpensive and reasonably good. English is widely (although not universally) spoken. The cost of living is very reasonable. This book is intended to meet the particular needs of the cruising yachtsman with a boat in the 10-20 meter range. It supplements (but is not intended to replace) conventional navigational materials, a discussion of which can be found below on page 16. I have tried to make this book accurate, but responsibility for the safety of your vessel and its crew must remain yours alone. CONVENTIONS IN THIS BOOK Coordinates are given for various features to help you find them on a chart, not for uncritical use with GPS. In most cases the position is approximate, and is only given to the nearest whole minute. Where coordinates are expressed more exactly, in decimal minutes or minutes and seconds, the relevant chart is mentioned or WGS 84 is the datum used. See the References section (page 157) for specific details of the chart edition used. -
Hurricane Flooding
ATM 10 Severe and Unusual Weather Prof. Richard Grotjahn L 18/19 http://canvas.ucdavis.edu Lecture 18 topics: • Hurricanes – what is a hurricane – what conditions favor their formation? – what is the internal hurricane structure? – where do they occur? – why are they important? – when are those conditions met? – what are they called? – What are their life stages? – What does the ranking mean? – What causes the damage? Time lapse of the – (Reading) Some notorious storms 2005 Hurricane Season – How to stay safe? Note the water temperature • Video clips (colors) change behind hurricanes (black tracks) (Hurricane-2005_summer_clouds-SST.mpg) Reading: Notorious Storms • Atlantic hurricanes are referred to by name. – Why? • Notorious storms have their name ‘retired’ © AFP Notorious storms: progress and setbacks • August-September 1900 Galveston, Texas: 8,000 dead, the deadliest in U.S. history. • September 1906 Hong Kong: 10,000 dead. • September 1928 South Florida: 1,836 dead. • September 1959 Central Japan: 4,466 dead. • August 1969 Hurricane Camille, Southeast U.S.: 256 dead. • November 1970 Bangladesh: 300,000 dead. • April 1991 Bangladesh: 70,000 dead. • August 1992 Hurricane Andrew, Florida and Louisiana: 24 dead, $25 billion in damage. • October/November 1998 Hurricane Mitch, Honduras: ~20,000 dead. • August 2005 Hurricane Katrina, FL, AL, MS, LA: >1800 dead, >$133 billion in damage • May 2008 Tropical Cyclone Nargis, Burma (Myanmar): >146,000 dead. Some Notorious (Atlantic) Storms Tracks • Camille • Gilbert • Mitch • Andrew • Not shown: – 2004 season (Charley, Frances, Ivan, Jeanne) – Katrina (Wilma & Rita) (2005) – Sandy (2012), Harvey (2017), Florence & Michael (2018) Hurricane Camille • 14-19 August 1969 • Category 5 at landfall – for 24 hours – peak winds 165 kts (190mph @ landfall) – winds >155kts for 18 hrs – min SLP 905 mb (26.73”) – 143 perished along gulf coast, – another 113 in Virginia Hurricane Andrew • 23-26 August 1992 • Category 5 at landfall • first Category 5 to hit US since Camille • affected S. -
Super Cyclone Yasa Hits Fiji Bringing Floods, Landslides Govt Warns Over 850,000 Fijians Are in the Direct Path of the Cyclone
18 Friday International Friday, December 18, 2020 Super cyclone Yasa hits Fiji bringing floods, landslides Govt warns over 850,000 Fijians are in the direct path of the cyclone SUVA: Super cyclone Yasa slammed into Fiji’s second-largest island struction wrought by Cyclone Winston in February 2016, which killed yesterday, tearing roofs off buildings as it triggered flash floods and 44 people and destroyed tens of thousands of homes. landslides in the Pacific island nation. After days of dire warnings about The Fijian leader, a long-time campaigner for climate action, blamed widespread destruction, Fiji’s Met service said the top-of-the-scale global warming for such super storms, which were once rare but have Category Five storm made landfall on Vanua Levu late yesterday pack- become relatively common. “As the world is getting warmer, these ing winds gusts of up to 345 kilometers an hour (210 miles an hour). It storms are getting stronger,” he said. “Every one of us must treat these Eight HK activists said the cyclone, one of the most powerful ever recorded in the South climate-fuelled catastrophes with deadly seriousness.” Pacific, would be accompanied by monster waves exceeding 10 meters charged over (33 feet). Yasa, which is expected to move out to sea early today, landed Lessons learned in the sparsely populated Bau province. There were no immediate re- Fiji has opened evacuation centers and people living near the coast ports of damage or casualties but social media posts showed flooded have been advised to flee to higher ground. Housing in Fiji’s villages is security law protest villages and corrugated sheeting blown off homes. -
Cyclone Ana – Fiji
ROTARY APPEAL FOR JANUARY 2021 CYCLONE ANA – FIJI FOLLOW UP REQUEST FOR DONATIONS OF CASH Just 7 weeks after Cyclone Yasa devastated Fiji resulting in some 345 ERKs being distributed, Fiji was struck by Cyclone Ana at the end of January. Whilst its intensity reached only Cat. 2, the rainfall before and since has been relentless. A further 600 ERKs have been released to the most vulnerable families in the Western Division. The cyclone season still has 10 weeks to run and we retain a small supply for another eventuality. The depletion of stock will require replenishment during the off season and our assembly team leaders have commenced putting a plan of action in place. Our appeal for donations following Cyclone Yasa was stricken by its timing coinciding with the Dec/Jan holidays. We are grateful to the clubs that did respond. It is now more than 35 years since Rotarians in Australia, New Zealand and elsewhere together with the NZ Govt. and the public began to provide first response support to our Pacific neighbours who almost annually are affected by cyclone, flood and on occasions tsunami. Rotary always collaborates with the New Zealand Ministry of Foreign Affairs Emergency Task Force in Wellington and the Emergency Disaster Management Office in country to ensure that the Emergency Response Kits and other supplies are directed for best possible advantage to those affected. Rotary and supporters provide logistical support where they are able, often themselves faced with destruction to their own homes. Retired NZHC endorses Rotary’s response. “I experienced first-hand the real value of the ERKS in 2012 in Samoa as New Zealand High Commissioner and as a member of the Apia Rotary Club. -
Long-Distance Nationalism: the Case of The
Long-distance nationalism: The case of the Pacific Islands’ Diaspora in Finland Samiuela Elone no. 012435786 Master’s Thesis Intercultural Encounters Faculty of Arts University of Helsinki May 2021 Supervisor Julie Yu-Wen Chen Tiedekunta – Fakultet – Faculty Koulutusohjelma – Utbildningsprogram: Degree Programme Humanistinen tiedekunta: Kulttuurienvälisen vuorovaikutuksen maisteriohjelma: Faculty of Arts Master’s Degree in Intercultural Encounters Opintosuunta – Studieinriktning – Study Track Master of Theology Tekijä – Författare – Author: Samiuela Elone Työn nimi – Arbetets titel – Title Long-distance nationalism: The case of the Pacific Islands’ diaspora in Finland Työn laji – Arbetets art – Level Pro Gradu- Aika – Datum – Month and year Sivumäärä– Sidoantal – Number of tutkielma – Master’s thesis May 2021 pages 62 + 22 Tiivistelmä - Referat – Abstract The Pacific islands’ diaspora consists of first-generation immigrants from different Pacific Island countries. In 2019, only 32 people living in Finland were born in the islands, ten of them participated in this study. Even though there have been studies on the Pacific Islands’ diasporas, this is the first time such a study has been conducted in Finland. It is also the first one of its kind to look at long-distance nationalism from the perspectives of the islanders in Finland. The three research questions are, how do the Pacific islanders forge and sustain a community in Finland? How do Pacific Islanders create and maintain connections with their homelands? What challenges do they face in their effort to reconnect with their homelands? The thesis tests three hypotheses; the islanders are creating a place and space for themselves “here” to belong, connect, and to practice their cultures; they maintain the connection to their home-islands through social media, sending remittances, and direct visit; there are factors, such as financial capital and personal changes, that inversely affect the islanders’ connectivity to their homelands. -
A Climatology of Tropical Cyclone Size in the Western North Pacific Using an Alternative Metric Thomas B
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2017 A Climatology of Tropical Cyclone Size in the Western North Pacific Using an Alternative Metric Thomas B. (Thomas Brian) McKenzie III Follow this and additional works at the DigiNole: FSU's Digital Repository. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES A CLIMATOLOGY OF TROPICAL CYCLONE SIZE IN THE WESTERN NORTH PACIFIC USING AN ALTERNATIVE METRIC By THOMAS B. MCKENZIE III A Thesis submitted to the Department of Earth, Ocean and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science 2017 Copyright © 2017 Thomas B. McKenzie III. All Rights Reserved. Thomas B. McKenzie III defended this thesis on March 23, 2017. The members of the supervisory committee were: Robert E. Hart Professor Directing Thesis Vasubandhu Misra Committee Member Jeffrey M. Chagnon Committee Member The Graduate School has verified and approved the above-named committee members, and certifies that the thesis has been approved in accordance with university requirements. ii To Mom and Dad, for all that you’ve done for me. iii ACKNOWLEDGMENTS I extend my sincere appreciation to Dr. Robert E. Hart for his mentorship and guidance as my graduate advisor, as well as for initially enlisting me as his graduate student. It was a true honor working under his supervision. I would also like to thank my committee members, Dr. Vasubandhu Misra and Dr. Jeffrey L. Chagnon, for their collaboration and as representatives of the thesis process. Additionally, I thank the Civilian Institution Programs at the Air Force Institute of Technology for the opportunity to earn my Master of Science degree at Florida State University, and to the USAF’s 17th Operational Weather Squadron at Joint Base Pearl Harbor-Hickam, HI for sponsoring my graduate program and providing helpful feedback on the research. -
Tropical Cyclones: Meteorological Aspects Mark A
Tropical Cyclones: Meteorological Aspects Mark A. Lander1 Water and Environmental Research Institute of the Western Pacific, University of Guam, UOG Station, Mangilao, Guam (USA) 96923 Sailors have long recognized the existence of deadly storms in Every year, TCs claim many lives—occasionally exceeding tropical latitudes where the weather was usually a mix of bright sun and 100,000. Some of the world’s greatest natural disasters have been gentle breezes with quickly passing showers. These terrifying storms associated with TCs. For example, Tropical Cyclone 02B was the were known to have a core of screaming winds accompanied by deadliest and most destructive natural disaster on earth in 1991. The blinding rain, spume and sea spray, and sharply lowered barometric associated extreme storm surge along the coast of Bangladesh was the pressure. When the sailors were lucky enough to survive penetration primary reason for the loss of 138,000 lives (Joint Typhoon Warning to the core of such violent weather, they found a region of calm. This Center, 1991). It occurred 19 years after the loss of ≈300,000 lives in region is the signature characteristic and best-known feature of these Bangladesh by a similar TC striking the low-lying Ganges River storms—the eye (Fig. 1). region in April 1970. In a more recent example, flooding caused by These violent storms of the tropical latitudes were known to be Hurricane Mitch killed 10,000+ people in Central America in Fall seasonal, hence their designation by Atlantic sailors as “line” storms, 1998. Nearly all tropical islands—the islands of the Caribbean, Ha- in reference to the sun’s crossing of the line (equator) in September (the waii, French Polynesia, Micronesia, Fiji, Samoa, Mauritius, La Re- month of peak hurricane activity in the North Atlantic). -
World Meteorological Organization Global Weather & Climate
ASU Home My ASU Colleges & Schools Map & Locations Directory SIGN IN Search World Meteorological Organization's World Weather & Climate Extremes Archive Weather Archive Home Recent Investigations Committee Record Assessment Related Links About Contact Home / Content / World Meteorological Organization Global Weather & Climate Extremes Archive World Meteorological Organization Global Weather & Climate Extremes Archive Global Weather & Climate Extremes # World Element Site Geopolitical Longitude/ World Weather Element Characteristic Value Date (D/M/Y) Observations Location Latitude Elevation Temperature Highest Temperature 56.7°C (134°F) 10/7 (July) /1913 1911- present Furnace Creek 36°27'N, -54m (Greenland Ranch), 116°51'W (-179ft) ) CA, USA Lowest Temperature -89.2°C 21/7 (July) /1983 1912- present Vostok, Antarctica 77°32'S, 3420m (-128.6°F) 106°40'E (11,220 ft) Pressure Highest Sea Lvl Air 1083.8 hPa 31/12 1961- present Agata, Russia 66°53'N, 261m Pressure Below 750m (December) 93°28'E (856.3ft) /1968 Highest Sea Lvl Air 1089.1 hPa 30/12 1963- present Tosontsengel 48°44'N, 1724.6m Pressure Above 750m (December) Mongolia 98°16'E (5658.1 ft) /2004 Lowest Sea Lvl Air 870 hPa 12/10 (October) 1951- present Eye of Typhoon Tip 16°44'N, 0m Pressure (excluding /1979 137°46'E tornadoes) Rainfall Greatest 1-Min Rainfall 31.2mm 4/7 (July) /1956 1948- present Unionville, MD, USA 38°48'N, 152m (1.23") 76°08'W (499ft) Greatest 60-Min Rainfall 305mm 22/6 (June) Holt, MO, USA 39°27'N, 263m (12.0") /1947 94°20'W (863ft) Greatest 12-Hr Rainfall 1.144 -
Pacific Cimate Change Migration and Human Security Programme
MARCH 2021 | ISSUE 002 ENHANCING PROTECTION AND EMPOWERMENT OF MIGRANTS AND COMMUNITIES AFFECTED BY CLIMATE CHANGE AND DISASTERS IN THE PACIFIC REGION PACIFIC CLIMATE CHANGE MIGRATION AND HUMAN SECURITY (PCCMHS) PROGRAMME QUARTERLY UPDATE © International Organization for Migration (IOM) UPDATE ON THE REGIONAL POLICY • The RPD presented government officials with DIALOGUE an opportunity to examine the challenges and opportunities to enhance protection of Pacific Islanders migrating in relation to climate change. Results of the RPD Some of the results of the RPD included: • exchanges and learning on the policies and measures adopted by individual Pacific countries to address challenges and harness opportunities related to climate mobility. • identification of opportunities to address the policy and legal gaps to enable protection of Pacific communities most prone to the impacts of the Left to right: Vakaoca Kedrayate (MOFA), Christopher Yee (IOM), Elenoa Patricia Momoivalu climate change. (ESCAP), Kristy Fong (MOFA), Mr. Iosefa Maiava, Head of UNESCAP Subregional Office for the Pacific, Mr. Esala Nayasi, Deputy Secretary Ministry of Foreign Affairs – Fiji, Alisi Vosalevu (PDD), Mr. Solomon Kantha, IOM Fiji Chief of Mission, Mr. Agus Wandi (RCO), Jone Tikoicolo (ESCAP), Sabira • Increased common understanding of the principles Coelho, PCCMHS Programme Manager, Shane Antonio (OHCHR). and objective of a regional framework to address climate mobility. Such a framework would be inclusive Recap of Regional Policy Dialogue of all voices, respectful of national experiences, and • From September – November 2020, a Regional anchored in existing political processes, Finally, Policy Dialogue (RPD) was organized virtually by it would aim to promote recognition and legal United Nations Economic and Social Commission protection of migrants and displaced persons, for Asia and the Pacific (ESCAP) with the support of particularly in the context of climate change. -
Tropical Cyclone: Climatology
ESCI 344 – Tropical Meteorology Lesson 5 – Tropical Cyclones: Climatology References: A Global View of Tropical Cyclones, Elsberry (ed.) The Hurricane, Pielke Tropical Cyclones: Their evolution, structure, and effects, Anthes Forecasters’ Guide to Tropical Meteorology, Atkinsson Forecasters Guide to Tropical Meteorology (updated), Ramage Global Guide to Tropical Cyclone Forecasting, Holland (ed.) Reading: Introduction to the Meteorology and Climate of the Tropics, Chapter 9 A Global View of Tropical Cyclones, Chapter 3 REQUIREMENTS FOR FORMATION In order for a tropical cyclone to form, the following general conditions must be present: Deep, warm ocean mixed layer. ◼ Sea-surface temperature at least 26.5C. ◼ Mixed layer depth of 45 meters or more. Relative maxima in absolute vorticity in the lower troposphere ◼ Need a preexisting cyclonic disturbance. ◼ Must be more than a few degrees of latitude from the Equator. Small values of vertical wind shear. ◼ Disturbance must be in deep easterly flow, or in a region of light upper- level winds. Mean upward vertical motion with humid mid-levels. GLOBAL CLIMATOLOGY Note: Most of the statistics given in this section are from Gray, W.M., 1985: Tropical Cyclone Global Climatology, WMO Technical Document WMO/TD-72, Vol. I, 1985. About 80 tropical cyclones per year world-wide reach tropical storm strength ( 34 kts). About 50 – 55 each year world-wide reach hurricane/typhoon strength ( 64 kts). The rate of occurrence globally is very steady. Global average annual variation is small (about 7%). Extreme variations are in the range of 16 to 22%. Variability within a particular region is much larger than global variability. Most (87%) form within 20 of the Equator. -
On Tropical Cyclones
Frequently Asked Questions on Tropical Cyclones Frequently Asked Questions on Tropical Cyclones 1. What is a tropical cyclone? A tropical cyclone (TC) is a rotational low-pressure system in tropics when the central pressure falls by 5 to 6 hPa from the surrounding and maximum sustained wind speed reaches 34 knots (about 62 kmph). It is a vast violent whirl of 150 to 800 km, spiraling around a centre and progressing along the surface of the sea at a rate of 300 to 500 km a day. The word cyclone has been derived from Greek word ‘cyclos’ which means ‘coiling of a snake’. The word cyclone was coined by Heary Piddington who worked as a Rapporteur in Kolkata during British rule. The terms "hurricane" and "typhoon" are region specific names for a strong "tropical cyclone". Tropical cyclones are called “Hurricanes” over the Atlantic Ocean and “Typhoons” over the Pacific Ocean. 2. Why do ‘tropical cyclones' winds rotate counter-clockwise (clockwise) in the Northern (Southern) Hemisphere? The reason is that the earth's rotation sets up an apparent force (called the Coriolis force) that pulls the winds to the right in the Northern Hemisphere (and to the left in the Southern Hemisphere). So, when a low pressure starts to form over north of the equator, the surface winds will flow inward trying to fill in the low and will be deflected to the right and a counter-clockwise rotation will be initiated. The opposite (a deflection to the left and a clockwise rotation) will occur south of the equator. This Coriolis force is too tiny to effect rotation in, for example, water that is going down the drains of sinks and toilets. -
Tropical Cyclone YASA
Emergency Response Coordination Centre (ERCC) – DG ECHO Daily Map | 17/12/2020 Fiji | Tropical Cyclone YASA SOLOMON TUVALU Tokelau 16 Dec 12:00 UTC ISLANDS (NEW ZEALAND) 259 km/h sust. winds Rotuma (FIJI) Nadogo SAMOA Vanua WALLIS AND AMERICAN Levu FUTUNA SAMOA Nukuira VANUATU 17 Dec Coral FIJI Sea NIUE TONGA Northern New Caledonia 131,914 (FRANCE) 17 Dec 06:00 UTC Exposed population to 241 km/h sust. winds winds ≥ 119 km/h*: SOUTH Vanua Levu PACIFIC OCEAN 160,000 people Western *Equivalent to category 1 or 337,041 Max wind speed higher, SSHS 17-19 Dec Source (GDACS) Vanua Source: Levu NOAA-HWRF, JRC ≥178 km/h SOUTH 17 Dec PACIFIC 17 Dec 18:00 UTC 06:00 UTC 119-177 km/h OCEAN 213 km/h sust. winds SOUTH 63-118 km/h PACIFIC Viti Levu OCEAN Tropical Cyclone (TC) Source: GDACS, JTWC FIJI FIJI Current position Central Past track Viti Levu 378,284 Forecast track 17 Dec 18:00 UTC Uncertainty cone Intensity Eastern î 119–259 km/h 37,648 Wind buffer ≥ 178 km/h Rotuma 119-177 km/h 18 Dec 06:00 UTC 1,583 185 km/h sust. winds Storm surge calculation 17-19 December SOUTH Source: JRC, atm. NOAA-HWRF PACIFIC OCEAN < 1 m 17 Dec 1-2.5 m Situation overview 3-day rainfall forecast ▪ National authorities, declared a State of Source: NOAA-HWRF Vanua Warnings Natural Disaster for all Fiji on 17 December. 25–50 mm Source: FMS Levu as of 17 December ▪ Landslides, flooding and power outages 50–00 mm have been reported across Central, Western 100–250 mm Hurricane and Northern Divisions.