Workshop on Tropical Cyclones and Climate
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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. -
Rapid Intensification of DOI:10.1175/BAMS-D-16-0134.1 Hurricanes Is Particularly Problematic
WILL GLOBAL WARMING MAKE HURRICANE FORECASTING MORE DIFFICULT? KERRY EMANUEL As the climate continues to warm, hurricanes may intensify more rapidly just before striking land, making hurricane forecasting more difficult. ince 1971, tropical cyclones have claimed about cyclone damage, rising on average 6% yr–1 in inflation- 470,000 lives, or roughly 10,000 lives per year, and adjusted U.S. dollars between 1970 and 2015 (CRED S caused 700 billion U.S. dollars in damages globally 2016). Thus, appreciable increases in forecast skill and/ (CRED 2016). Mortality is strongly dominated by a or decreases of vulnerability, for example, through small number of extremely lethal events; for example, better preparedness, building codes, and evacuation just three storms caused more than 56% of the tropical procedures, will be required to avoid increases in cyclone–related deaths in the United States since 1900. cyclone-related casualties. Tropical cyclone mortality and injury have been Unfortunately, there has been little improvement reduced by improved forecasts and preparedness, espe- in tropical cyclone intensity forecasts over the period cially in developed countries (Arguez and Elsner 2001; from 1990 to the present (DeMaria et al. 2014). While Peduzzi et al. 2012), but through much of the world hurricane track forecasts using numerical prediction this has been offset by large changes in coastal popula- models have steadily improved, there has been only tions. For example, Peduzzi et al. (2012) estimate that slow improvement in forecasts of intensity by these the global population exposed to tropical cyclone same models. Reasons for this include stiff resolu- hazards increased by almost threefold between 1970 tion requirements for the numerical simulations of and 2010, and they project this trend to continue for tropical cyclone intensity (Rotunno et al. -
Machine Learning of Atmospheric Turbulence in a Variational Multiscale Model Msc Thesis
Machine Learning of Atmospheric Turbulence in a Variational Multiscale Model MSc Thesis Martin Janssens Machine Learning of Atmospheric Turbulence in a Variational Multiscale Model MSc Thesis by Martin Janssens to obtain the degree of Master of Science at the Delft University of Technology, to be defended publicly on Tuesday August 27, 2019 at 10:00 AM. Student number: 4275780 Project duration: September 16, 2018 – August 28, 2019 Supervisor: Dr. S. J. Hulshoff, TU Delft Thesis committee: Dr. R. P.Dwight, TU Delft Dr. B. Chen, TU Delft An electronic version of this thesis is available at http://repository.tudelft.nl/. Cover image: The Starry Night, Vincent van Gogh Abstract Today’s leading projections of climate change predicate on atmospheric General Circulation Models (GCMs). Since the atmosphere consists of a staggering range of scales that impact global trends, but computational constraints prevent many of these scales from being directly represented in numerical simulations, GCMs require “parameterisations” - models for the influence of unresolved processes on the resolved scales. State- of-the-art parameterisations are commonly based on combinations of phenomenological arguments and physics, and are of considerably lower fidelity than the resolved simulation. In particular, the parameter- isation of low-altitude stratocumulus clouds that result from small-scale processes in sub-tropical marine boundary layers is widely considered the largest source of uncertainty that remains in contemporary GCMs’ prediction of the temperature response to a global increase in CO2. Improvements in the capacity of machine learning algorithms and the increasing availability of high- fidelity datasets from global satellite data and local Large Eddy Simulations (LES) have identified data-driven parameterisations as a high-potential option to break the deadlock. -
Textremes Forms the Paths of NCM014
Evaluation of the contribution of tropical cyclone seeds to changes in tropical cyclone frequency due to global warming in high-resolution multi-model ensemble simulations Article Published Version Creative Commons: Attribution 4.0 (CC-BY) Open Access Yamada, Y. ORCID: https://orcid.org/0000-0001-6092-9944, Kodama, C., Satoh, M., Sugi, M., Roberts, M. J., Mizuta, R., Noda, A. T., Nasuno, T., Nakano, M. and Vidale, P. L. (2021) Evaluation of the contribution of tropical cyclone seeds to changes in tropical cyclone frequency due to global warming in high-resolution multi-model ensemble simulations. Progress in Earth and Planetary Science, 8 (1). ISSN 2197-4284 doi: https://doi.org/10.1186/s40645-020-00397-1 Available at http://centaur.reading.ac.uk/98236/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . Published version at: http://dx.doi.org/10.1186/s40645-020-00397-1 To link to this article DOI: http://dx.doi.org/10.1186/s40645-020-00397-1 Publisher: Springer All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online Yamada et al. Progress in Earth and Planetary Science (2021) 8:11 Progress in Earth and https://doi.org/10.1186/s40645-020-00397-1 Planetary Science RESEARCH ARTICLE Open Access Evaluation of the contribution of tropical cyclone seeds to changes in tropical cyclone frequency due to global warming in high-resolution multi-model ensemble simulations Yohei Yamada1* , Chihiro Kodama1, Masaki Satoh2, Masato Sugi3, Malcolm J. -
Climate Science and Climate Risk: a Primer
Climate Science and Climate Risk: A Primer By Dr. Kerry A. Emanuel Professor of Atmospheric Science Massachusetts Institute of Technology email: [email protected] website: http://eaps4.mit.edu/faculty/Emanuel/ Dr. Kerry A. Emanuel | Climate Science and Climate Risk: A Primer 1 Considerably more than 90% percent of climate scientists attribute the bulk of the increase in global mean temperature over the past three to four decades to the anthropogenic increase in atmospheric greenhouse gases that commenced with the Industrial Revolution.1 The great majority of these scientists hold that continued warming presents significant risks to humankind over the coming centuries. What scientific evidence led the scientific community to these conclusions? How robust is that evidence? To what extent should we trust uncertain projections of future climate change based on complicated global climate models? How do we deal with climate change as a problem of risk assessment and management? his essay summarizes the most important lines of not fit within the existing scientific framework. Scientists T evidence for anthropogenic climate change, confronts then try to repeat and improve on the observation to some of the stickier questions behind uncertainty in determine whether it really is an outlier. Next, they may pose climate projections, and concludes with a discussion of the one or more hypotheses to explain the observation, and if a particular risks entailed by climate change and how they are hypothesis succeeds in explaining not only that observation being quantified. but others as well, and especially if it successfully predicts The essay is structured as follows. First, a brief history of what has not yet been observed, the hypothesis may advance climate science reveals that the most important principles to the status of a theory. -
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. -
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. -
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 ........................................................................................................................................... -
Climate Changes Associated with Increasing CO 2
Welcome to ATMS 111 Global Warming http://www.atmos.washington.edu/2010Q1/111 These slides are preliminary and will likely be revised by class time. Vertical structure of the atmosphere Stratosphere ozone layer / ozone hole ultraviolet solar radiation sulfate aerosols from volcanic eruptions increasing GHG produces cooling Troposphere most clouds and atmospheric water vapor ozone from air pollution short residence time of aerosols Hurricanes and other storms RG p128-146 A taste of things to come? Keeping count: will there be more cyclones in the future? Surges and downpours Coastal concerns beyond the tropics Coastal storm flooding: a deepening problem Tornadoes: an overblown connection? Was Hurricane Katrina related to global warming? http://orca.rsmas.miami.edu/~schen/Isabel/goes_floater030912.avi Photo by UW Prof R. Houze The first storm churns up colder, deeper waters and leaves a trail of cool in its wake. The second storm loses strength when intersects this cold water trail. NASA NASA's Aqua and TRMM of SST. Sea height using the Jason-1 satellite. http://www.nasa.gov/centers/goddard/earthandsun/eye_to_eye.html Another example of cooler SST after storm passes Cold ocean temperature in Katrina’s Wake http://www.gfdl.noaa.gov/visualizations-hurricanes Loop Current 200-300km wide 80-150 m deep warm current ribbon In step 2 it has stretched so that it breaks off an eddy in step 3 Happens about ~6-11 months http://www7320.nrlssc.navy.mil/global_nlom32/ias.html Hurricane Katrina: Ocean Heat Content and wind speed in mph (next to black dots) Hurricane produce oceanic upwelling beneath the eye Upwelling of cold water can provide a strong negative feedback that limits the strength of the hurricane. -
IUGG03-Program.Pdf
The Science Council of Japan and sixteen Japanese scientific societies will host IUGG2003, the XXIII General Assembly of the International Union of Geodesy and Geophysics. Hosts Science Council of Japan The Geodetic Society of Japan Seismological Society of Japan The Volcanological Society of Japan Meteorological Society of Japan Society of Geomagnetism and Earth, Planetary and Space Sciences Japan Society of Hydrology and Water Resources The Japanese Association of Hydrological Sciences The Japanese Society of Snow and Ice The Oceanographic Society of Japan The Japanese Society for Planetary Sciences The Japanese Society of Limnology Japan Society of Civil Engineers Japanese Association of Groundwater Hydrology The Balneological Society of Japan Japan Society of Erosion Control Engineering The Geochemical Society of Japan Special Support Hokkaido Prefecture City of Sapporo Co-Sponsor National Research Institute for Earth Science and Disaster Prevention (JSS01 Hagiwara Symposium on Monitoring and Modeling of Earthquake and Volcanic Processes for Prediction) Center for Climate System Research, University of Tokyo (JSM01 Toward High Resolution Climate Models and Earth System Models) Support Ministry of Education, Culture, Sports, Science and Technology Ministry of Economy, Trade and Industry Ministry of Land, Infrastructure and Transport Japan Marine Science and Technology Center National Institute of Advanced Industrial Science and Technology Japan Earth and Planetary Science Joint Meeting Organization Japanese Forestry Society Japan Business -
The San Diego Hurricane of 2 October 1858
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 Tsouthwestern 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. -
Hurricanes: Tempests in a Greenhouse Kerry Emanuel
Hurricanes: Tempests in a greenhouse Kerry Emanuel quick Greenhouse gases make Earth’s surface hotter than it would be if the study planet were simply a blackbody radiator. That additional warming is an important driver of hurricanes. Kerry Emanuel is a professor of atmospheric sciences at the Massachusetts Institute of Technology in Cambridge, Massachusetts. The tropics have generally the most benign climates found ated with precipitation absorb most of the entropy produc- on Earth, with gentle breezes and small daily and seasonal tion and spare people from violent winds. But not always. temperature variations. Why, then, do tropical climates breed the most destructive wind storms known? This brief tutorial A Carnot engine explains the paradox and presents an overview of hurricane In the part of the tropics where the sea surface is warm physics. enough and the projection of Earth’s angular velocity vector onto the local vertical axis is large enough, random small- The greenhouse effect scale convective currents sometimes organize into rotating Of the solar energy that streams to Earth, about 30% is re- vortices known as tropical cyclones. In computer models of flected by clouds or the surface, and an additional small per- the tropical atmosphere, such organization can happen spon- centage is directly absorbed by atmospheric water—either taneously, but usually only if a combination of ocean tem- gaseous or condensed in clouds. The radiation that escapes perature and rotation is somewhat higher than those ob- reflection or absorption in the atmosphere is absorbed by the served in nature. In subcritical conditions, some trigger is surface, which transmits energy upward both by radiation necessary to initiate the vortices, and in the terrestrial at- and in vast convective currents whose visible manifestations mosphere tropical cyclones only develop from preexisting are the beautiful cumulus and cumulonimbus clouds that ply disturbances of independent origin.