Atmospheric Research 2014 Technical Highlights
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Homeowners Handbook to Prepare for Natural Disasters
HOMEOWNERS HANDBOOK HANDBOOK HOMEOWNERS DELAWARE HOMEOWNERS TO PREPARE FOR FOR TO PREPARE HANDBOOK TO PREPARE FOR NATURAL HAZARDSNATURAL NATURAL HAZARDS TORNADOES COASTAL STORMS SECOND EDITION SECOND Delaware Sea Grant Delaware FLOODS 50% FPO 15-0319-579-5k ACKNOWLEDGMENTS This handbook was developed as a cooperative project among the Delaware Emergency Management Agency (DEMA), the Delaware Department of Natural Resources and Environmental Control (DNREC) and the Delaware Sea Grant College Program (DESG). A key priority of this project partnership is to increase the resiliency of coastal communities to natural hazards. One major component of strong communities is enhancing individual resilience and recognizing that adjustments to day-to- day living are necessary. This book is designed to promote individual resilience, thereby creating a fortified community. The second edition of the handbook would not have been possible without the support of the following individuals who lent their valuable input and review: Mike Powell, Jennifer Pongratz, Ashley Norton, David Warga, Jesse Hayden (DNREC); Damaris Slawik (DEMA); Darrin Gordon, Austin Calaman (Lewes Board of Public Works); John Apple (Town of Bethany Beach Code Enforcement); Henry Baynum, Robin Davis (City of Lewes Building Department); John Callahan, Tina Callahan, Kevin Brinson (University of Delaware); David Christopher (Delaware Sea Grant); Kevin McLaughlin (KMD Design Inc.); Mark Jolly-Van Bodegraven, Pam Donnelly and Tammy Beeson (DESG Environmental Public Education Office). Original content from the first edition of the handbook was drafted with assistance from: Mike Powell, Greg Williams, Kim McKenna, Jennifer Wheatley, Tony Pratt, Jennifer de Mooy and Morgan Ellis (DNREC); Ed Strouse, Dave Carlson, and Don Knox (DEMA); Joe Thomas (Sussex County Emergency Operations Center); Colin Faulkner (Kent County Department of Public Safety); Dave Carpenter, Jr. -
Winter Precipitation Liquid–Ice Phase Transitions Revealed with Polarimetric Radar and 2DVD Observations in Central Oklahoma
MAY 2017 B U K O V CICETAL. 1345 Winter Precipitation Liquid–Ice Phase Transitions Revealed with Polarimetric Radar and 2DVD Observations in Central Oklahoma PETAR BUKOVCIC ´ NOAA/National Severe Storms Laboratory, and Cooperative Institute for Mesoscale Meteorological Studies, and School of Meteorology, and Advanced Radar Research Center, University of Oklahoma, Norman, Oklahoma DUSAN ZRNIC´ NOAA/National Severe Storms Laboratory, Norman, Oklahoma GUIFU ZHANG School of Meteorology, and Advanced Radar Research Center, University of Oklahoma, Norman, Oklahoma (Manuscript received 30 June 2016, in final form 8 November 2016) ABSTRACT Observations and analysis of an ice–liquid phase precipitation event, collected with an S-band polarimetric KOUN radar and a two-dimensional video disdrometer (2DVD) in central Oklahoma on 20 January 2007, are presented. Using the disdrometer measurements, precipitation is classified either as ice pellets or rain/freezing rain. The disdrometer observations showed fast-falling and slow-falling particles of similar size. The vast majority (.99%) were fast falling with observed velocities close to those of raindrops with similar sizes. In contrast to the smaller particles (,1 mm in diameter), bigger ice pellets (.1.5 mm) were relatively easy to distinguish because their shapes differ from the raindrops. The ice pellets were challenging to detect by looking at conventional polarimetric radar data because of the localized and patchy nature of the ice phase and their occurrence close to the ground. Previously published findings referred to cases in which ice pellet areas were centered on the radar location and showed a ringlike structure of enhanced differential reflectivity ZDR and reduced copolar correlation coefficient rhv and horizontal reflectivity ZH in PPI images. -
Downloaded 10/01/21 08:52 PM UTC 186 WEATHER and FORECASTING VOLUME 16
FEBRUARY 2001 NOTES AND CORRESPONDENCE 185 Further Investigation of a Physically Based, Nondimensional Parameter for Discriminating between Locations of Freezing Rain and Ice Pellets ROBERT M. RAUBER,LARRY S. OLTHOFF, AND MOHAN K. RAMAMURTHY Department of Atmospheric Sciences, University of Illinois at Urbana±Champaign, Urbana, Illinois KENNETH E. KUNKEL Midwestern Climate Center, Illinois State Water Survey, Champaign, Illinois 9 December 1999 and 16 August 2000 ABSTRACT The general applicability of an isonomogram developed by Czys and coauthors to diagnose the position of the geographic boundary between freezing precipitation (freezing rain or freezing drizzle) and ice pellets (sleet or snow grains) was tested using a 25-yr sounding database consisting of 1051 soundings, 581 where stations were reporting freezing drizzle, 391 reporting freezing rain, and 79 reporting ice pellets. Of the 1051 soundings, only 306 clearly had an environmental temperature and moisture pro®le corresponding to that assumed for the isonomogram. This pro®le consisted of a three-layer atmosphere with 1) a cold cloud layer aloft that is a source of ice particles, 2) a midlevel layer where the temperature exceeds 08C and ice particles melt, and 3) a surface layer where T , 08C. The remaining soundings did not conform to the pro®le either because 1) the freezing precipitation was associated with the warm rain process or 2) the ice pellets formed due to riming rather than melting and refreezing. For soundings conforming to the pro®le, the isonomogram showed little diagnostic skill. Freezing rain or freezing drizzle occurred about 50% of the time that ice pellets were expected. -
NASA Sees Ex-Tropical Cyclone Gillian's Remnants Persist 20 March 2014
NASA sees ex-Tropical Cyclone Gillian's remnants persist 20 March 2014 (PR) instrument revealed that intense convective storms in this area were still dropping rain at a rate of over 97 mm/3.8 inches per hour and returning radar reflectivity values of over 51dBZ. TRMM PR data were used to create a simulated 3-D view that showed the vertical structure of precipitation within the stormy area contained towering thunderstorms. The Joint Typhoon Warning Center noted that animated enhanced satellite imagery on March 20 showed flaring deep convection associated with a slowly-consolidating low-level circulation center. On March 20, the Tropical Cyclone Warning Centre in Jakarta noted that Gillian's remnants had maximum sustained winds near 25 knots/28.7 mph/46.3 kph. It was centered near 9.4 south and 119.0 east, about 233 nautical miles/ 268.1 miles/431.5 km east of South Kuta, Bali, Indonesia. TRMM passed above Gillian's remnants on March 20, TCWC issued watches and warnings for parts of 2014, and this 3-D simulation of TRMM data showed the Indonesia archipelago in Bahasa. several of the tallest thunderstorms in Gillian's remnants were reaching heights of over 15.75 km/9.8 miles. Credit: NASA/SSAI, Hal Pierce NASA's TRMM satellite continues to follow the remnants of former Tropical Cyclone Gillian as it moved from the Southern Pacific Ocean into the Southern Indian Ocean where it appears to be re- organizing. The persistent remnants of tropical cyclone Gillian have moved westward over 2,700 km/1,674 miles since forming in the Gulf of Carpentaria on March 8, 2014. -
Summary of 2013 Atlantic Seasonal Tropical Cyclone Activity And
SUMMARY OF 2013 ATLANTIC TROPICAL CYCLONE ACTIVITY AND VERIFICATION OF AUTHORS' SEASONAL AND TWO-WEEK FORECASTS The 2013 Atlantic hurricane season was much quieter than predicted in our seasonal outlooks. While many of the large-scale conditions typically associated with active seasons were present (e.g., anomalously warm tropical Atlantic, absence of El Niño conditions, anomalously low tropical Atlantic sea level pressures), very dry mid-level air combined with mid-level subsidence and stable lapse rates to significantly suppress the 2013 Atlantic hurricane season. These unfavorable conditions were likely generated by a significant weakening of our proxy for the strength of the Atlantic Multi-Decadal Oscillation/Atlantic Thermohaline Circulation during the late spring into the early summer. Overall activity in 2013 was approximately 30% of the 1981-2010 median. By Philip J. Klotzbach1 and William M. Gray2 This forecast as well as past forecasts and verifications are available via the World Wide Web at http://hurricane.atmos.colostate.edu Kortny Rolston, Colorado State University Media Representative, (970-491-5349) is available to answer various questions about this verification. Department of Atmospheric Science Colorado State University Fort Collins, CO 80523 Email: [email protected] As of 19 November 2013 1 Research Scientist 2 Professor Emeritus of Atmospheric Science 1 ATLANTIC BASIN SEASONAL HURRICANE FORECASTS FOR 2013* Forecast Parameter and 1981-2010 Median 10 April 2013 Update Update Observed % of 1981- (in parentheses) -
News and Notes
346 BULLETIN AMERICAN METEOROLOGICAL SOCIETY NEWS AND NOTES Air Force Scientists Develop Technique The feasibility of dissipating supercooled clouds by for Cutting Holes in "Cold" Clouds seeding with dry-ice was recognized many years ago. Airborne equipment, previously developed to do this, A new technique for creating holes in supercooled cloud crushed large blocks of dry-ice into particles suitable for layers has been developed by Air Force Cambridge Re- seeding purposes. search Laboratories scientists. During recent flight tests This equipment had two particular limitations. First, using this technique, holes more than 3 miles wide were these machines produced about half powdered dry-ice created in supercooled clouds. which evaporated immediately upon dispersal from the Major James F. Church, project scientist in AFCRL's aircraft and was wasted. Second, the logistical problem Meteorological Research Laboratory is directing research of supplying enough dry-ice where needed and the high on the dissipation of supercooled stratiform clouds. The evaporational losses suffered during storage until used, program is under the technical management of the Air severely limited the utility of this technique. Force System Command's Electronic Systems Division. The Cloudbuster makes ice pellets by passing liquid The principal objective of this research is to provide C02 through an expansion nozzle and then compacting Air Force cargo and transport pilots with an economical the solid dry-ice powder, which is then formed, into proper capability to seed supercooled clouds with dry-ice pellets, size. The Cloudbuster has been designed with the capa- made on the aircraft and dispersed at will, to create bility of making different-sized pellets at the touch of a sizable holes in such cloud decks. -
National Hurricane Operations Plan
U.S. DEPARTMENT OF COMMERCE/ National Oceanic and Atmospheric Administration OFFICE OF THE FEDERAL COORDINATOR FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH National Hurricane Operations Plan FCM-P12-2015 Washington, DC May 2015 THE INTERDEPARTMENTAL COMMITTEE FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH (ICMSSR) MR. DAVID McCARREN, CHAIR MR. PAUL FONTAINE Acting Federal Coordinator Federal Aviation Administration Department of Transportation MR. MARK BRUSBERG Department of Agriculture DR. JONATHAN M. BERKSON United States Coast Guard DR. LOUIS UCCELLINI Department of Homeland Security Department of Commerce DR. DAVID R. REIDMILLER MR. SCOTT LIVEZEY Department of State United States Navy Department of Defense DR. ROHIT MATHUR Environmental Protection Agency MR. RALPH STOFFLER United States Air Force DR. EDWARD CONNER Department of Defense Federal Emergency Management Agency Department of Homeland Security MR. RICKEY PETTY Department of Energy DR. RAMESH KAKAR National Aeronautics and Space MR. JOEL WALL Administration Science and Technology Directorate Department of Homeland Security DR. PAUL B. SHEPSON National Science Foundation MR. JOHN VIMONT Department of the Interior MR. DONALD E. EICK National Transportation Safety Board MR. MARK KEHRLI Federal Highway Administration MR. SCOTT FLANDERS Department of Transportation U.S. Nuclear Regulatory Commission MR. MICHAEL C. CLARK Office of Management and Budget MR. MICHAEL BONADONNA, Secretariat Office of the Federal Coordinator for Meteorological Services and Supporting Research Cover Image NOAA GOES-13, 15 October 2014; Hurricane Gonzalo; Credit: NOAA Environmental Visualization Laboratory FEDERAL COORDINATOR FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH 1325 East-West Highway, Suite 7130 Silver Spring, Maryland 20910 301-628-0112 http://www.ofcm.gov/ NATIONAL HURRICANE OPERATIONS PLAN http://www.ofcm.gov/nhop/15/nhop15.htm FCM-P12-2015 Washington, D.C. -
METAR/SPECI Reporting Changes for Snow Pellets (GS) and Hail (GR)
U.S. DEPARTMENT OF TRANSPORTATION N JO 7900.11 NOTICE FEDERAL AVIATION ADMINISTRATION Effective Date: Air Traffic Organization Policy September 1, 2018 Cancellation Date: September 1, 2019 SUBJ: METAR/SPECI Reporting Changes for Snow Pellets (GS) and Hail (GR) 1. Purpose of this Notice. This Notice coincides with a revision to the Federal Meteorological Handbook (FMH-1) that was effective on November 30, 2017. The Office of the Federal Coordinator for Meteorological Services and Supporting Research (OFCM) approved the changes to the reporting requirements of small hail and snow pellets in weather observations (METAR/SPECI) to assist commercial operators in deicing operations. 2. Audience. This order applies to all FAA and FAA-contract weather observers, Limited Aviation Weather Reporting Stations (LAWRS) personnel, and Non-Federal Observation (NF- OBS) Program personnel. 3. Where can I Find This Notice? This order is available on the FAA Web site at http://faa.gov/air_traffic/publications and http://employees.faa.gov/tools_resources/orders_notices/. 4. Cancellation. This notice will be cancelled with the publication of the next available change to FAA Order 7900.5D. 5. Procedures/Responsibilities/Action. This Notice amends the following paragraphs and tables in FAA Order 7900.5. Table 3-2: Remarks Section of Observation Remarks Section of Observation Element Paragraph Brief Description METAR SPECI Volcanic eruptions must be reported whenever first noted. Pre-eruption activity must not be reported. (Use Volcanic Eruptions 14.20 X X PIREPs to report pre-eruption activity.) Encode volcanic eruptions as described in Chapter 14. Distribution: Electronic 1 Initiated By: AJT-2 09/01/2018 N JO 7900.11 Remarks Section of Observation Element Paragraph Brief Description METAR SPECI Whenever tornadoes, funnel clouds, or waterspouts begin, are in progress, end, or disappear from sight, the event should be described directly after the "RMK" element. -
The Mesoscale Dynamics of Freezing Rain Storms Over Eastern Canada
VOL. 56, NO.10 JOURNAL OF THE ATMOSPHERIC SCIENCES 15 MAY 1999 The Mesoscale Dynamics of Freezing Rain Storms over Eastern Canada K. K. SZETO Climate Processes and Earth Observation Division, Atmospheric Environment Service, Downsview, Ontario, Canada A. TREMBLAY Cloud Physics Research Division, Atmospheric Environment Service, Dorval, Quebec, Canada H. GUAN AND D. R. HUDAK Cloud Physics Research Division, Atmospheric Environment Service, Downsview, Ontario, Canada R. E. STEWART AND Z. CAO Climate Processes and Earth Observation Division, Atmospheric Environment Service, Downsview, Ontario, Canada (Manuscript received 2 June 1997, in ®nal form 9 June 1998) ABSTRACT A severe ice storm affected the east coast of Canada during the Canadian Atlantic Storms Project II. A hierarchy of cloud-resolving model simulations of this storm was performed with the objective of enhancing understanding of the cloud and mesoscale processes that affected the development of freezing rain events. The observed features of the system were reasonably well replicated in the high-resolution simulation. Diagnosis of the model results suggests that the change of surface characteristics from ocean to land when the surface warm front approaches Newfoundland disturbs the (quasi-) thermal wind balance near the frontal region. The cross-frontal circulation intensi®es in response to the thermal wind imbalance, which in turn leads to the development of an extensive above-freezing inversion layer in the model storm. Depending on the depth of the subfreezing layer below the inversion, the melted snow may refreeze within the subfreezing layer to form ice pellets or they may refreeze at the surface to form freezing rain. Such evolution of surface precipitation types in the model storm was reasonably well simulated in the model. -
Nur Wenige Atlantik-Hurrikane in Der Saison 2013*) Werner Wehry
Beiträge zur Berliner Wetterkarte Herausgegeben vom Verein BERLINER WETTERKARTE e.V. zur Förderung der meteorologischen Wissenschaft c/o Institut für Meteorologie der Freien Universität Berlin, C.-H.-Becker-Weg 6-10, 12165 Berlin 62/13 http://www.Berliner-Wetterkarte.de ISSN 0177-3984 SO 23/13 11.12.2013 Nur wenige Atlantik-Hurrikane in der Saison 2013*) Werner Wehry Seit einigen Jahren geben der britische (UKMetOffice) und der amerikanische (NOAA) Wetterdienst im Frühjahr Vorhersagen über den Verlauf, die Stärke und die Anzahl der tropischen Wettersysteme über dem Nordatlantik heraus. Im Folgenden werden zunächst die Prognosen vom UKMetOffice, dann die von NOAA für 2013 vorgestellt. Abb. 1a (links oben): Vorhersage des UKMetOffice, ausgegeben am 15.5.2013. Hierzu heißt es: "Die wahrscheinlichste Anzahl tropischer Stürme über dem Nordatlantik zwischen Juni und November" (2013) "liegt bei 14, wobei mit 70%iger Wahrscheinlichkeit zwischen 10 und 18 auftreten werden. Dies entspricht einer leicht übernormalen Aktivität im Vergleich zum Mittel von 12 der Jahre 1980 bis 2012." Abb. 1b (rechts oben): "Die wahrscheinlichste Anzahl von Hurrikanen über dem Nordatlantik zwischen Juni und November" (2013) "liegt bei 9, wobei mit 70%iger Wahrscheinlichkeit zwischen 4 und 14 auftreten werden. Dies entspricht einer leicht übernormalen Aktivität im Vergleich zum Mittel von 6 der Jahre1980 bis 2012." Abb. 1c (links unten): Der wahrscheinlichste summierte zyklonale Energie-Index (ACE, s. folgende Seite) von 130 ist für Juni bis November 2013 vorhergesagt, wobei der Index mit 70%iger Wahr- scheinlichkeit zwischen 76 und 184 liegen wird, was etwas über dem Mittel von 104 der Jahre 1980 bis 2012 liegt." http://www.metoffice.gov.uk/weather/tropicalcyclone/seasonal/northatlantic2013 *) Siehe auch Beilage Nr. -
The 2010-12 Drought and Subsequent Extensive Flooding © Front Cover Images: Flooding at Exbridge, December 2012, Heather Lowther, CEH
National Hydrological Monitoring Programme ISBN 978-1-906698-44-7 The 2010-12 drought and subsequent extensive flooding © Front cover images: Flooding at Exbridge, December 2012, Heather Lowther, CEH. - a remarkable hydrological transformation Drought at Hurtswood Reservoir, © United Utilities. Design: Centre for Ecology & Hydrology. by Terry Marsh, Simon Parry, Mike Kendon & Jamie Hannaford Printed on Forest Stewardship Council (FSC) approved recycled papers, from well-managed forests and other controlled sources. National Hydrological Monitoring Programme The 2010-12 drought and subsequent extensive flooding - a remarkable hydrological transformation by Terry Marsh, Simon Parry, Mike Kendon & Jamie Hannaford CENTRE FOR ECOLOGY & HYDROLOGY l [email protected] l www.ceh.ac.uk [i] This report should be cited as Marsh, T.J.1, Parry, S.1, Kendon, M.C.2, and Hannaford, J.1 2013. The 2010-12 drought and subsequent extensive flooding. Centre for Ecology & Hydrology. 54 pages. Affiliations: 1Centre for Ecology & Hydrology; 2Met Office. ISBN: 978-1-906698-44-7 Publication Address Centre for Ecology & Hydrology Maclean Building Benson Lane Crowmarsh Gifford Wallingford Oxfordshire OX10 8BB UK General and business enquiries: +44 (0)1491 838800 E-mail: [email protected] Cover design: Heather Lowther [ii] The 2010-12 drought and subsequent extensive flooding - a remarkable hydrological transformation THE 2010-12 DROUGHT AND SUBSEQUENT EXTENSIVE FLOODING – A REMARKABLE HYDROLOGICAL TRANSFORMatION The work for this report was carried out by scientists from the Centre for Ecology & Hydrology (CEH), the UK’s centre of excellence for research in land and freshwater environmental sciences in partnership with the Met Office; technical guidance was provided by the British Geological Survey (BGS), the UK’s premier centre for earth science information and expertise. -
Smoke Haze Trigger Factors in the Malaysia Indonesian Border
Utopía y Praxis Latinoamericana ISSN: 1315-5216 ISSN: 2477-9555 [email protected] Universidad del Zulia Venezuela Smoke Haze Trigger Factors in the Malaysia Indonesian Border MUADI, SHOLIH Smoke Haze Trigger Factors in the Malaysia Indonesian Border Utopía y Praxis Latinoamericana, vol. 26, no. Esp.1, 2021 Universidad del Zulia, Venezuela Available in: https://www.redalyc.org/articulo.oa?id=27966119036 DOI: https://doi.org/10.5281/zenodo.4556305 This work is licensed under Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International. PDF generated from XML JATS4R by Redalyc Project academic non-profit, developed under the open access initiative SHOLIH MUADI. Smoke Haze Trigger Factors in the Malaysia Indonesian Border Artículos Smoke Haze Trigger Factors in the Malaysia Indonesian Border Factores desencadenantes de la neblina de humo en la frontera de Malasia e Indonesia SHOLIH MUADI DOI: https://doi.org/10.5281/zenodo.4556305 Brawijaya University, Indonesia Redalyc: https://www.redalyc.org/articulo.oa? [email protected] id=27966119036 https://orcid.org/0000-0002-9263-5526 Received: 12 December 2020 Accepted: 15 February 2021 Abstract: e purpose of this study was to analyze the haze incidence and trigger factors at the border between Indonesia and Malaysia. e results of the study reveal that the Biggest Factor Triggering the Haze Disaster is that forest and land fires are mostly caused by human behavior, whether intentional or as a result of negligence. Only a small part is caused by nature (lightning or volcanic lava). In the event of forest fires and natural disasters, 99% of incidents in Indonesia are caused by human factors, either intentionally or negligently.