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Synthesis and Assessment Product 1.3
CCSP 1.3 April 2, 2008 1 2 3 U.S. Climate Change Science Program 4 5 6 Synthesis and Assessment Product 1.3 7 8 Reanalysis of Historical Climate 9 Data for Key Atmospheric Features: 10 Implications for Attribution of 11 Causes of Observed Change 12 13 14 15 Lead Agency: 16 National Oceanic and Atmospheric Administration 17 18 Contributing Agencies: 19 Department of Energy 20 National Aeronautics and Space Administration 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 Note to Reviewers: This report has not yet undergone rigorous copy-editing 36 and will do so prior to layout for publication Do Not Cite or Quote 1 of 332 Public Review Draft CCSP 1.3 April 2, 2008 1 Table of Contents 2 3 ABSTRACT .................................................................................................................................................. 5 4 PREFACE..................................................................................................................................................... 7 5 P.1 OVERVIEW OF REPORT............................................................................................................... 7 6 P.2 PRIMARY REPORT FOCI.............................................................................................................. 9 7 P.2.1 Reanalysis of Historical Climate Data for Key Atmospheric Features................................... 10 8 P.2.2 Attribution of the Causes of Climate Variations and Trends Over North America ............... 11 9 P.3 TREATMENT OF UNCERTAINTY............................................................................................ -
Soaring Weather
Chapter 16 SOARING WEATHER While horse racing may be the "Sport of Kings," of the craft depends on the weather and the skill soaring may be considered the "King of Sports." of the pilot. Forward thrust comes from gliding Soaring bears the relationship to flying that sailing downward relative to the air the same as thrust bears to power boating. Soaring has made notable is developed in a power-off glide by a conven contributions to meteorology. For example, soar tional aircraft. Therefore, to gain or maintain ing pilots have probed thunderstorms and moun altitude, the soaring pilot must rely on upward tain waves with findings that have made flying motion of the air. safer for all pilots. However, soaring is primarily To a sailplane pilot, "lift" means the rate of recreational. climb he can achieve in an up-current, while "sink" A sailplane must have auxiliary power to be denotes his rate of descent in a downdraft or in come airborne such as a winch, a ground tow, or neutral air. "Zero sink" means that upward cur a tow by a powered aircraft. Once the sailcraft is rents are just strong enough to enable him to hold airborne and the tow cable released, performance altitude but not to climb. Sailplanes are highly 171 r efficient machines; a sink rate of a mere 2 feet per second. There is no point in trying to soar until second provides an airspeed of about 40 knots, and weather conditions favor vertical speeds greater a sink rate of 6 feet per second gives an airspeed than the minimum sink rate of the aircraft. -
11Th Australian Space Forum Wednesday 31 March 2021 Adelaide, South Australia
11th Australian Space Forum Wednesday 31 March 2021 Adelaide, South Australia 11th Australian Space Forum a 11th Australian Space Forum Wednesday 31 March 2021 Adelaide, South Australia Major Sponsor Supported by b 11th Australian Space Forum c Contents Welcome from the Chair of The Andy Thomas Space Foundation The Andy Thomas Space Foundation is delighted to welcome you to the 11th Australian Space Forum. Contents 11th Australian Space Forum The Foundation will be working with partners Wednesday 31 March 2021 1 Welcome and sponsors, including the Australian Space Adelaide, South Australia — Chair of The Andy Thomas Agency, on an ambitious agenda of projects Space Foundation to advance space education and outreach. Adelaide Convention Centre, — Premier of South Australia We are reaching out to friends and supporters North Terrace, Adelaide, South Australia — Head of the Australian who have a shared belief in the power of Forum sessions: Hall C Space Agency education, the pursuit of excellence and a Exhibition: Hall H commitment to diversity and inclusion. We 6 Message from the CEO The Foundation was established in 2020 for look forward to conversations during the 8 Forum Schedule the purpose of advancing space education, Forum – as well as ongoing interaction - about raising space awareness and contributing our shared interests and topics of importance 11 Speaker Profiles to the national space community. We to the national space community. are delighted that the South Australian 28 Company Profiles We hope you enjoy the 11th Australian Government has entrusted us with the future Space Forum. 75 Foundation Corporate Sponsors conduct of the Australian Space Forum – and Professional Partners Australia’s most significant space industry Michael Davis AO meeting – and we intend to ensure that the Chair, Andy Thomas Space Foundation 76 Venue Map Forum continues to be the leading national 77 Exhibition Floorplan platform for the highest quality information and discussion about space industry topics. -
Cloud Characteristics, Thermodynamic Controls and Radiative Impacts During the Observations and Modeling of the Green Ocean Amazon (Goamazon2014/5) Experiment
Atmos. Chem. Phys., 17, 14519–14541, 2017 https://doi.org/10.5194/acp-17-14519-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Cloud characteristics, thermodynamic controls and radiative impacts during the Observations and Modeling of the Green Ocean Amazon (GoAmazon2014/5) experiment Scott E. Giangrande1, Zhe Feng2, Michael P. Jensen1, Jennifer M. Comstock1, Karen L. Johnson1, Tami Toto1, Meng Wang1, Casey Burleyson2, Nitin Bharadwaj2, Fan Mei2, Luiz A. T. Machado3, Antonio O. Manzi4, Shaocheng Xie5, Shuaiqi Tang5, Maria Assuncao F. Silva Dias6, Rodrigo A. F de Souza7, Courtney Schumacher8, and Scot T. Martin9 1Environmental and Climate Sciences Department, Brookhaven National Laboratory, Upton, NY, USA 2Pacific Northwest National Laboratory, Richland, WA, USA 3National Institute for Space Research, São José dos Campos, Brazil 4National Institute of Amazonian Research, Manaus, Amazonas, Brazil 5Lawrence Livermore National Laboratory, Livermore, CA, USA 6University of São Paulo, São Paulo, Department of Atmospheric Sciences, Brazil 7State University of Amazonas (UEA), Meteorology, Manaus, Brazil 8Texas A&M University, College Station, Department of Atmospheric Sciences, TX, USA 9Harvard University, Cambridge, School of Engineering and Applied Sciences and Department of Earth and Planetary Sciences, MA, USA Correspondence to: Scott E. Giangrande ([email protected]) Received: 12 May 2017 – Discussion started: 24 May 2017 Revised: 30 August 2017 – Accepted: 11 September 2017 – Published: 6 December 2017 Abstract. Routine cloud, precipitation and thermodynamic 1 Introduction observations collected by the Atmospheric Radiation Mea- surement (ARM) Mobile Facility (AMF) and Aerial Facility The simulation of clouds and the representation of cloud (AAF) during the 2-year US Department of Energy (DOE) processes and associated feedbacks in global climate mod- ARM Observations and Modeling of the Green Ocean Ama- els (GCMs) remains the largest source of uncertainty in zon (GoAmazon2014/5) campaign are summarized. -
Sea State in Marine Safety Information Present State, Future Prospects
Sea State in Marine Safety Information Present State, future prospects Henri SAVINA – Jean-Michel LEFEVRE Météo-France Rogue Waves 2004, Brest 20-22 October 2004 JCOMM Joint WMO/IOC Commission for Oceanography and Marine Meteorology The future of Operational Oceanography Intergovernmental body of technical experts in the field of oceanography and marine meteorology, with a mandate to prepare both regulatory (what Member States shall do) and guidance (what Member States should do) material. TheThe visionvision ofof JCOMMJCOMM Integrated ocean observing system Integrated data management State-of-the-art technologies and capabilities New products and services User responsiveness and interaction Involvement of all maritime countries JCOMM structure Terms of Reference Expert Team on Maritime Safety Services • Monitor / review operations of marine broadcast systems, including GMDSS and others for vessels not covered by the SOLAS convention •Monitor / review technical and service quality standards for meteo and oceano MSI, particularly for the GMDSS, and provide assistance and support to Member States • Ensure feedback from users is obtained through appropriate channels and applied to improve the relevance, effectiveness and quality of services • Ensure effective coordination and cooperation with organizations, bodies and Member States on maritime safety issues • Propose actions as appropriate to meet requirements for international coordination of meteorological and related communication services • Provide advice to the SCG and other Groups of JCOMM on issues related to MSS Chair selected by Commission. OPEN membership, including representatives of the Issuing Services for GMDSS, of IMO, IHO, ICS, IMSO, and other user groups GMDSS Global Maritime Distress & Safety System Defined by IMO for the provision of MSI and the coordination of SAR alerts on a global basis. -
NWS Unified Surface Analysis Manual
Unified Surface Analysis Manual Weather Prediction Center Ocean Prediction Center National Hurricane Center Honolulu Forecast Office November 21, 2013 Table of Contents Chapter 1: Surface Analysis – Its History at the Analysis Centers…………….3 Chapter 2: Datasets available for creation of the Unified Analysis………...…..5 Chapter 3: The Unified Surface Analysis and related features.……….……….19 Chapter 4: Creation/Merging of the Unified Surface Analysis………….……..24 Chapter 5: Bibliography………………………………………………….…….30 Appendix A: Unified Graphics Legend showing Ocean Center symbols.….…33 2 Chapter 1: Surface Analysis – Its History at the Analysis Centers 1. INTRODUCTION Since 1942, surface analyses produced by several different offices within the U.S. Weather Bureau (USWB) and the National Oceanic and Atmospheric Administration’s (NOAA’s) National Weather Service (NWS) were generally based on the Norwegian Cyclone Model (Bjerknes 1919) over land, and in recent decades, the Shapiro-Keyser Model over the mid-latitudes of the ocean. The graphic below shows a typical evolution according to both models of cyclone development. Conceptual models of cyclone evolution showing lower-tropospheric (e.g., 850-hPa) geopotential height and fronts (top), and lower-tropospheric potential temperature (bottom). (a) Norwegian cyclone model: (I) incipient frontal cyclone, (II) and (III) narrowing warm sector, (IV) occlusion; (b) Shapiro–Keyser cyclone model: (I) incipient frontal cyclone, (II) frontal fracture, (III) frontal T-bone and bent-back front, (IV) frontal T-bone and warm seclusion. Panel (b) is adapted from Shapiro and Keyser (1990) , their FIG. 10.27 ) to enhance the zonal elongation of the cyclone and fronts and to reflect the continued existence of the frontal T-bone in stage IV. -
11 General Circulation
Copyright © 2017 by Roland Stull. Practical Meteorology: An Algebra-based Survey of Atmospheric Science. v1.02 “Practical Meteorology: An Algebra-based Survey of Atmospheric Science” by Roland Stull is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. View this license at http://creativecommons.org/licenses/by- nc-sa/4.0/ . This work is available at https://www.eoas.ubc.ca/books/Practical_Meteorology/ 11 GENERAL CIRCULATION Contents A spatial imbalance between radiative inputs and outputs exists for the earth-ocean-atmosphere 11.1. Key Terms 330 system. The earth loses energy at all latitudes due 11.2. A Simple Description of the Global Circulation 330 to outgoing infrared (IR) radiation. Near the trop- 11.2.1. Near the Surface 330 ics, more solar radiation enters than IR leaves, hence 11.2.2. Upper-troposphere 331 there is a net input of radiative energy. Near Earth’s 11.2.3. Vertical Circulations 332 poles, incoming solar radiation is too weak to totally 11.2.4. Monsoonal Circulations 333 offset the IR cooling, allowing a net loss of energy. 11.3. Radiative Differential Heating 334 The result is differential heating, creating warm 11.3.1. North-South Temperature Gradient 335 equatorial air and cold polar air (Fig. 11.1a). 11.3.2. Global Radiation Budgets 336 This imbalance drives the global-scale general 11.3.3. Radiative Forcing by Latitude Belt 338 circulation of winds. Such a circulation is a fluid- 11.3.4. General Circulation Heat Transport 338 dynamical analogy to Le Chatelier’s Principle of 11.4. -
Headland Sediment Bypassing Processes
UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS HEADLAND SEDIMENT BYPASSING PROCESSES Doutoramento em Geologia Especialidade em Geodinâmica Externa Mónica Sofia Afonso Ribeiro Tese orientada por: Professor Doutor Rui Pires de Matos Taborda Doutora Aurora da Conceição Coutinho Rodrigues Bizarro Documento especialmente elaborado para a obtenção do grau de doutor 2017 UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS HEADLAND SEDIMENT BYPASSING PROCESSES Doutoramento em Geologia Especialidade em Geodinâmica Externa Mónica Sofia Afonso Ribeiro Tese orientada por: Professor Doutor Rui Pires de Matos Taborda Doutora Aurora da Conceição Coutinho Rodrigues Bizarro Júri: Presidente: ● Doutora Maria da Conceição Pombo de Freitas Vogais: ● Doutor António Henrique da Fontoura Klein ● Doutor Óscar Manuel Fernandes Cerveira Ferreira ● Doutora Anabela Tavares Campos Oliveira ● Doutor César Augusto Canelhas Freire de Andrade ● Doutor Rui Pires de Matos Taborda Documento especialmente elaborado para a obtenção do grau de doutor Fundação para a Ciência e Tecnologia, no âmbito da Bolsa de Doutoramento com a referência SFRH/BD/79126/2011 2017 Em memória do meu irmão Luís Acknowledgments | Agradecimentos O doutoramento é um processo exigente, por vezes solitário, mas que só é possível com o apoio e a colaboração de outras pessoas e instituições. Portanto, resta-me agradecer a todos os que contribuíram para a conclusão deste trabalho. Em primeiro lugar agradeço aos meus orientadores, Rui Taborda e Aurora Bizarro, que têm acompanhado o meu trabalho desde os meus primeiros passos na Geologia Marinha, já lá vão 10 anos! A eles agradeço o incentivo para iniciar este projeto, o apoio demonstrado em todas as fases do trabalho, a confiança e a amizade. Ao Rui agradeço, em particular, a partilha e discussão de ideias e os desafios constantes que me permitiram evoluir. -
North Pacific Ocean
468 ¢ U.S. Coast Pilot 7, Chapter 11 31 MAY 2020 Chart Coverage in Coast Pilot 7—Chapter 11 124° NOAA’s Online Interactive Chart Catalog has complete chart coverage 18480 http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml 126° 125° Cape Beale V ANCOUVER ISLAND (CANADA) 18485 Cape Flattery S T R A I T O F Neah Bay J U A N D E F U C A Cape Alava 18460 48° Cape Johnson QUILLAYUTE RIVER W ASHINGTON HOH RIVER Hoh Head 18480 QUEETS RIVER RAFT RIVER Cape Elizabeth QUINAULT RIVER COPALIS RIVER Aberdeen 47° GRAYS HARBOR CHEHALIS RIVER 18502 18504 Willapa NORTH PA CIFIC OCEAN WILLAPA BAY South Bend 18521 Cape Disappointment COLUMBIA RIVER 18500 Astoria 31 MAY 2020 U.S. Coast Pilot 7, Chapter 11 ¢ 469 Columbia River to Strait of Juan De Fuca, Washington (1) This chapter describes the Pacific coast of the State (15) of Washington from the Washington-Oregon border at the ENCs - US3WA03M, US3WA03M mouth of the Columbia River to the northwesternmost Chart - 18500 point at Cape Flattery. The deep-draft ports of South Bend and Raymond, in Willapa Bay, and the deep-draft ports of (16) From Cape Disappointment, the coast extends Hoquiam and Aberdeen, in Grays Harbor, are described. north for 22 miles to Willapa Bay as a low sandy beach, In addition, the fishing port of La Push is described. The with sandy ridges about 20 feet high parallel with the most outlying dangers are Destruction Island and Umatilla shore. Back of the beach, the country is heavily wooded. -
NP 2013.Docx
LISTE INTERNATIONALE DES NOMS PROTÉGÉS (également disponible sur notre Site Internet : www.IFHAonline.org) INTERNATIONAL LIST OF PROTECTED NAMES (also available on our Web site : www.IFHAonline.org) Fédération Internationale des Autorités Hippiques de Courses au Galop International Federation of Horseracing Authorities 15/04/13 46 place Abel Gance, 92100 Boulogne, France Tel : + 33 1 49 10 20 15 ; Fax : + 33 1 47 61 93 32 E-mail : [email protected] Internet : www.IFHAonline.org La liste des Noms Protégés comprend les noms : The list of Protected Names includes the names of : F Avant 1996, des chevaux qui ont une renommée F Prior 1996, the horses who are internationally internationale, soit comme principaux renowned, either as main stallions and reproducteurs ou comme champions en courses broodmares or as champions in racing (flat or (en plat et en obstacles), jump) F de 1996 à 2004, des gagnants des neuf grandes F from 1996 to 2004, the winners of the nine épreuves internationales suivantes : following international races : Gran Premio Carlos Pellegrini, Grande Premio Brazil (Amérique du Sud/South America) Japan Cup, Melbourne Cup (Asie/Asia) Prix de l’Arc de Triomphe, King George VI and Queen Elizabeth Stakes, Queen Elizabeth II Stakes (Europe/Europa) Breeders’ Cup Classic, Breeders’ Cup Turf (Amérique du Nord/North America) F à partir de 2005, des gagnants des onze grandes F since 2005, the winners of the eleven famous épreuves internationales suivantes : following international races : Gran Premio Carlos Pellegrini, Grande Premio Brazil (Amérique du Sud/South America) Cox Plate (2005), Melbourne Cup (à partir de 2006 / from 2006 onwards), Dubai World Cup, Hong Kong Cup, Japan Cup (Asie/Asia) Prix de l’Arc de Triomphe, King George VI and Queen Elizabeth Stakes, Irish Champion (Europe/Europa) Breeders’ Cup Classic, Breeders’ Cup Turf (Amérique du Nord/North America) F des principaux reproducteurs, inscrits à la F the main stallions and broodmares, registered demande du Comité International des Stud on request of the International Stud Book Books. -
Analysis of a Southerly Buster Event and Associated Solitary Waves
CSIRO PUBLISHING Journal of Southern Hemisphere Earth Systems Science, 2019, 69, 205–215 https://doi.org/10.1071/ES19015 Analysis of a southerly buster event and associated solitary waves Shuang WangA,B,D, Lance LeslieA, Tapan RaiA, Milton SpeerA and Yuriy KuleshovC AUniversity of Technology Sydney, Sydney, NSW, Australia. BBureau of Meteorology, PO Box 413, Darlinghurst, NSW 1300, Australia. CBureau of Meteorology, Melbourne, Vic., Australia. DCorresponding author. Email: [email protected] Abstract. This paper is a detailed case study of the southerly buster of 6–7 October 2015, along the New South Wales coast. It takes advantage of recently available Himawari-8 high temporal- and spatial-resolution satellite data, and other observational data. The data analyses support the widespread view that the southerly buster is a density current, coastally trapped by the Great Dividing Range. In addition, it appeared that solitary waves developed in this event because the prefrontal boundary layer was shallow and stable. A simplified density current model produced speeds matching well with observational southerly buster data, at both Nowra and Sydney airports. Extending the density current theory, to include inertia-gravity effects, suggested that the solitary waves travel at a speed of ,20% faster than the density current. This speed difference was consistent with the high-resolution satellite data, which shows the solitary waves moving increasingly ahead of the leading edge of the density current. Additional keywords: coastally trapped disturbance, density currents. Received 19 May 2019, accepted 7 October 2019, published online 11 June 2020 1 Introduction speed of ,20 m/s at the leading edge of the ridge (Holland and Southerly busters (SBs) occur during the spring and summer Leslie 1986). -
Dicionarioct.Pdf
McGraw-Hill Dictionary of Earth Science Second Edition McGraw-Hill New York Chicago San Francisco Lisbon London Madrid Mexico City Milan New Delhi San Juan Seoul Singapore Sydney Toronto Copyright © 2003 by The McGraw-Hill Companies, Inc. All rights reserved. Manufactured in the United States of America. Except as permitted under the United States Copyright Act of 1976, no part of this publication may be repro- duced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written permission of the publisher. 0-07-141798-2 The material in this eBook also appears in the print version of this title: 0-07-141045-7 All trademarks are trademarks of their respective owners. Rather than put a trademark symbol after every occurrence of a trademarked name, we use names in an editorial fashion only, and to the benefit of the trademark owner, with no intention of infringement of the trademark. Where such designations appear in this book, they have been printed with initial caps. McGraw-Hill eBooks are available at special quantity discounts to use as premiums and sales promotions, or for use in corporate training programs. For more information, please contact George Hoare, Special Sales, at [email protected] or (212) 904-4069. TERMS OF USE This is a copyrighted work and The McGraw-Hill Companies, Inc. (“McGraw- Hill”) and its licensors reserve all rights in and to the work. Use of this work is subject to these terms. Except as permitted under the Copyright Act of 1976 and the right to store and retrieve one copy of the work, you may not decom- pile, disassemble, reverse engineer, reproduce, modify, create derivative works based upon, transmit, distribute, disseminate, sell, publish or sublicense the work or any part of it without McGraw-Hill’s prior consent.