Grade 12 Geography Climatology Answer Book
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Air Masses and Fronts
CHAPTER 4 AIR MASSES AND FRONTS Temperature, in the form of heating and cooling, contrasts and produces a homogeneous mass of air. The plays a key roll in our atmosphere’s circulation. energy supplied to Earth’s surface from the Sun is Heating and cooling is also the key in the formation of distributed to the air mass by convection, radiation, and various air masses. These air masses, because of conduction. temperature contrast, ultimately result in the formation Another condition necessary for air mass formation of frontal systems. The air masses and frontal systems, is equilibrium between ground and air. This is however, could not move significantly without the established by a combination of the following interplay of low-pressure systems (cyclones). processes: (1) turbulent-convective transport of heat Some regions of Earth have weak pressure upward into the higher levels of the air; (2) cooling of gradients at times that allow for little air movement. air by radiation loss of heat; and (3) transport of heat by Therefore, the air lying over these regions eventually evaporation and condensation processes. takes on the certain characteristics of temperature and The fastest and most effective process involved in moisture normal to that region. Ultimately, air masses establishing equilibrium is the turbulent-convective with these specific characteristics (warm, cold, moist, transport of heat upwards. The slowest and least or dry) develop. Because of the existence of cyclones effective process is radiation. and other factors aloft, these air masses are eventually subject to some movement that forces them together. During radiation and turbulent-convective When these air masses are forced together, fronts processes, evaporation and condensation contribute in develop between them. -
Extreme Climatic Characteristics Near the Coastline of the Southeast Region of Brazil in the Last 40 Years
Extreme Climatic Characteristics Near the Coastline of the Southeast Region of Brazil in the Last 40 Years Marilia Mitidieri Fernandes de Oliveira ( [email protected] ) Federal University of Rio de Janeiro: Universidade Federal do Rio de Janeiro Jorge Luiz Fernandes de Oliveira Fluminense Federal University Pedro José Farias Fernandes Fluminense Federal University, Physical Geography Laboratory (LAGEF), Eric Gilleland National, Center for Atmospheric Research (NCAR) Nelson Francisco Favilla Ebecken Federal University of Rio de Janeiro: Universidade Federal do Rio de Janeiro Research Article Keywords: ERA5 Reanalysis data, Non-parametric statistical tests, severe weather systems, subtropical cyclones Posted Date: June 7th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-159473/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License 1 Extreme climatic characteristics near the coastline of the Southeast region of Brazil in the last 40 years Marilia Mitidieri Fernandes de Oliveira1, Jorge Luiz Fernandes de Oliveira2, Pedro José Farias Fernandes3, Eric Gilleland4, Nelson Francisco Favilla Ebecken1 1Federal University of Rio de Janeiro, Civil Engineering Postgraduate Program-COPPE/UFRJ, Center of Technology, Rio de Janeiro 21945-970, Brazil 2Fluminense Federal University, Geography Postgraduate Program, Department of Geography, Geoscience Institute, Niterói 24210-340, Brazil 3Fluminense Federal University, Physical Geography Laboratory (LAGEF), Department of Geography, Niterói 24210-340, -
NOTES and CORRESPONDENCE Synoptic-Scale Controls of Summer
15 FEBRUARY 2006 NOTES AND CORRESPONDENCE 613 NOTES AND CORRESPONDENCE Synoptic-Scale Controls of Summer Precipitation in the Southeastern United States JEREMY E. DIEM Department of Anthropology and Geography, Georgia State University, Atlanta, Georgia (Manuscript received 15 October 2004, in final form 11 August 2005) ABSTRACT Past climatological research has not quantitatively defined the synoptic-scale circulation deviations re- sponsible for anomalous summer-season precipitation totals in the southeastern United States. Therefore, the objectives of this research were to determine the synoptic-scale controls of wet and dry multiday periods during the summer within a portion of the southeastern United States as well as to assess the linkages between synoptic-scale circulation and multidecadal variations in precipitation characteristics for the study domain. Daily precipitation data from 30 stations for June, July, and August from 1953 to 2002 were converted into 13-day totals. Using standardized principal components analysis (PCA), the study domain was divided into three precipitation regions (i.e., South, Northwest, and Northeast). Wet and dry periods for each region were composed of the top 56 and bottom 56 thirteen-day periods. Composite circulation maps for 500 and 850 mb revealed the following: wet periods were generally associated with an upper-level trough over the interior southeastern United States coincident with strong lower-tropospheric flow into the South- east from the Gulf of Mexico, and dry periods were characterized by ridges or anticyclones over the midwestern and southeastern United States coupled with weak lower-tropospheric flow. Many of the wet periods had surface fronts. Over the 50-yr period, increased precipitation was significantly correlated with increased occurrences of midtropospheric troughs over the study domain. -
1 Climatology of South American Seasonal Changes
Vol. 27 N° 1 y 2 (2002) 1-30 PROGRESS IN PAN AMERICAN CLIVAR RESEARCH: UNDERSTANDING THE SOUTH AMERICAN MONSOON Julia Nogués-Paegle 1 (1), Carlos R. Mechoso (2), Rong Fu (3), E. Hugo Berbery (4), Winston C. Chao (5), Tsing-Chang Chen (6), Kerry Cook (7), Alvaro F. Diaz (8), David Enfield (9), Rosana Ferreira (4), Alice M. Grimm (10), Vernon Kousky (11), Brant Liebmann (12), José Marengo (13), Kingste Mo (11), J. David Neelin (2), Jan Paegle (1), Andrew W. Robertson (14), Anji Seth (14), Carolina S. Vera (15), and Jiayu Zhou (16) (1) Department of Meteorology, University of Utah, USA, (2) Department of Atmospheric Sciences, University of California, Los Angeles, USA, (3) Georgia Institute of Technology; Earth & Atmospheric Sciences, USA (4) Department of Meteorology, University of Maryland, USA, (5) Laboratory for Atmospheres, NASA/Goddard Space Flight Center, USA, (6) Department of Geological and Atmospheric Sciences, Iowa State University, USA, (7) Department of Earth and Atmospheric Sciences, Cornell University, USA, (8) Instituto de Mecánica de Fluidos e Ingeniería Ambiental, Universidad de la República, Uruguay, (9) NOAA Atlantic Oceanographic Laboratory, USA, (10) Department of Physics, Federal University of Paraná, Brazil, (11) Climate Prediction Center/NCEP/NWS/NOAA, USA, (12) NOAA-CIRES Climate Diagnostics Center, USA, (13) Centro de Previsao do Tempo e Estudos de Clima, CPTEC, Brazil, (14) International Research Institute for Climate Prediction, Lamont Doherty Earth Observatory of Columbia University, USA, (15) CIMA/Departmento de Ciencias de la Atmósfera, University of Buenos Aires, Argentina, (16) Goddard Earth Sciences Technology Center, University of Maryland, USA. (Manuscript received 13 May 2002, in final form 20 January 2003) ABSTRACT A review of recent findings on the South American Monsoon System (SAMS) is presented. -
Synoptic-Scale Controls of Fog and Low Clouds in the Namib Desert: Response to Reviewer 1
Synoptic-scale controls of fog and low clouds in the Namib Desert: Response to Reviewer 1 Hendrik Andersen, Jan Cermak, Julia Fuchs, Peter Knippertz, Marco Gaetani, Julian Quinting, Sebastian Sippel, and Roland Vogt contact: [email protected] We would like to thank reviewer 1 for her/his careful review of the manuscript and her/his constructive criticism and valuable comments. Comments by the referee are colored in black, our replies or comments are colored in blue and italics. Using a 14-year period of reanalysis grids and backward trajectories, this study examines the impact of large-scale dynamics and thermodynamics on fog and low clouds (FLCs) over Namib. Specifically, the authors’ focus on two seasons when different FLC types are observed due to different synoptic-scale regimes. A main finding is that the mean sea level pressure (MSLP) field differs notably between clear and FLC days. To this end, the authors’ use a statistical model and MSLP fields to provide skillful prediction of FLCs up to one day in advance. A new conceptual model of the two different FLC regimes is developed to summarize findings and aid in future studies related to FLCs over Namib. In general, the scientific purpose is justified, the findings are important, and the paper is well-written; however, I do have concerns about some of the methods used. Overall, I think that the results are interesting and worthy of publication, and at this stage I suggest acceptance subject to major revisions. Major/general comments: 1. Use of MSLP, 2 m temperature, and 10 m winds to characterize synoptic-scale conditions This study relies on the assumption that near-surface (boundary layer) meteorological variables – specifically MSLP, 2 m temperature, and 10 m horizontal wind components – are representative of the large-scale dynamics. -
Weather, Current and Routing Brief the Clipper 11/12 Round the World
Weather, Current and Routing Brief The Clipper 11/12 Round the World Race Prepared for the Race Skippers by Simon Rowell 27th April 2011 1. Leg One - Europe to Rio de Janeiro (early August to mid September) 4 1.1. The Route 4 1.2. The Weather 6 1.2.1. The Iberian Peninsula to the Canaries 6 1.2.2. The Canaries 10 1.2.3. The Canaries to the ITCZ, via the Cape Verdes 11 1.2.4. The ITCZ in the Atlantic 13 1.2.5. The ITCZ to Cabo Frio 16 1.3. Currents 18 1.3.1. The Iberian Peninsula to the Equator 18 1.3.2. The Equator to Rio 20 2. Leg 2 – Rio de Janeiro to Cape Town (mid September to mid October) 22 2.1. The Route 22 2.2. The Weather 22 2.3. Currents 27 3. Leg 3 – Cape Town to Western Australia (October to November) 29 3.1. The Route 29 3.2. The Weather 30 3.2.1. Southern Indian Ocean Fronts 34 3.3. Currents 35 3.3.1 Currents around the Aghulas Bank 35 3.3.2 Currents in the Southern Indian Ocean 37 4. Leg 4 –Western Australia to Wellington to Eastern Australia (mid November to December) 4.1. The Route 38 4.2. The Weather 39 4.2.1. Cape Leeuwin to Tasmania 39 4.2.2. Tasmania to Wellington and then to Gold Coast 43 4.3. Currents 47 5. Leg 5 – Gold Coast to Singapore to Qingdao (early January to end of February) 48 5.1. -
Geography P1 November 2019 Marking Guidelines
NATIONAL SENIOR CERTIFICATE GRADE 12 GEOGRAPHY P1 NOVEMBER 2019 MARKING GUIDELINES MARKS: 225 These marking guidelines consist of 26 pages. Copyright reserved Please turn over Geography/P1 2 DBE/November 2019 NSC – Marking Guidelines Marking Guidelines The following marking guidelines have been developed to standardise marking in all provinces. Marking • ALL selected questions MUST be marked, irrespective of whether it is correct or incorrect • Candidates are expected to make a choice of THREE questions to answer. If all questions are answered, ONLY the first three questions are marked. • A clear, neat tick must be used: o If ONE mark is allocated, ONE tick must be used: o If TWO marks are allocated, TWO ticks must be used: o The tick must be placed at the FACT that a mark is being allocated for o Ticks must be kept SMALL, as various layers of moderation may take place • Incorrect answers must be marked with a clear, neat cross: o Use MORE than one cross across a paragraph/discussion style questions to indicate that all facts have been considered o Do NOT draw a line through an incorrect answer o Do NOT underline the incorrect facts • Where the maximum marks have been allocated in the first few sentences of a paragraph, place an M over the remainder of the text to indicate the maximum marks have been achieved For the following action words, ONE word answers are acceptable: give, list, name, state, identify For the following action words, a FULL sentence must be written: describe, explain, evaluate, analyse, suggest, differentiate, -
Study & Master Geography Grade 12 Teacher's Guide
Ge0graphy CAPS Grade Teacher’s Guide Helen Collett • Norma Catherine Winearls Peter J Holmes 12 SM_Geography_12_TG_CAPS_ENG.indd 1 2013/06/11 6:21 PM Study & Master Geography Grade 12 Teacher’s Guide Helen Collett • Norma Catherine Winearls • Peter J Holmes SM_Geography_12_TG_TP_CAPS_ENGGeog Gr 12 TG.indb 1 BW.indd 1 2013/06/116/11/13 7:13:30 6:09 PMPM CAMBRIDGE UNIVERSITY PRESS Cambridge, New York, Melbourne, Madrid, Cape Town, Singapore, São Paulo, Delhi, Mexico City Cambridge University Press The Water Club, Beach Road, Granger Bay, Cape Town 8005, South Africa www.cup.co.za © Cambridge University Press 2013 This publication is in copyright. Subject to statutory exception and to the provisions of relevant collective licensing agreements, no reproduction of any part may take place without the written permission of Cambridge University Press. First published 2013 ISBN 978-1-107-38162-9 Editor: Barbara Hutton Proofreader: Anthea Johnstone Artists: Sue Abraham and Peter Holmes Typesetter: Brink Publishing & Design Cover image: Gallo Images/Wolfgang Poelzer/Getty Images ………………………………………………......…………………………………………………………… ACKNOWLEDGEMENTS Photographs: Peter Holmes: pp. 267, 271, 273 and 274 Maps: Chief Directorate: National Geo-spatial Information: Department of Rural Development and Land Reform: pp. 189, 233–235 and 284–289 ………………………………………………......…………………………………………………………… Cambridge University Press has no responsibility for the persistence or accuracy of URLs for external or third-party internet websites referred to in this publication, and does not guarantee that any content on such websites is, or will remain, accurate or appropriate. Information regarding prices, travel timetables and other factual information given in this work are correct at the time of first printing but Cambridge University Press does not guarantee the accuracy of such information thereafter. -
North and South American Low-Level Jets
American Low Level jetS A Scientific Prospectus and Implementation Plan North and South American Low-Level Jets Draft, March 2001 Prepared by Julia Nogues-Paegle and Jan Paegle (University of Utah, USA) with con- tributions from Michael Douglas (NOAA/NSSL, USA), Matilde Nicolini, Carolina Vera (University of Buenos Aires, Argentina), Jose Marengo (CPTEC, Brazil), Rene Garreaud (University of Chile, Chile), James Shuttleworth (University of Arizona, USA), C. Roberto Mechoso (UCLA, USA) and E. Hugo Berbery (University of Mary- land, USA). TABLE OF CONTENTS Executive Summary 5 1. What is the ALLS program? 6 2. Why the American Jets? 9 3. Science Objectives 11 3.1 Identify LLJ events and variability 11 3.1.1. North America 11 3.1.2. South America 14 3.2 Quantify LLJ contributions to the hydrological cycle 16 3.2.1. North America 16 3.2.2. South America 17 3.3 Determine plateau effects 19 3.3.1. North America 19 3.3.2. South America 19 3.4 Develop and validate theories on LLJ generation and variability 21 3.4.1. North America 21 3.4.2. South America 22 3.4.3 Local and remote influences on ALLS in relation 23 to droughts and floods 4. Implementation Plan 26 4.1 Numerical Modelling 26 4.2 Diagnostic Studies 29 4.3 Field Component of ALLS 30 4.3.1. Region of focus for the ALLS South American Field Program 32 4.3.2. Radiosonde network 33 4.3.3. Pilot balloon observations 35 4.3.4. Wind profiler observations 35 4.3.5. -
Meteorological Glossary
METEOROLOGICAL GLOSSARY Met. O. 842 A.P.897 Meteorological Office Meteorological Glossary Compiled by D. H. Mclntosh, M.A., D.Sc. London: Her Majesty's Stationery Office: 1972 U.D.C. 551.5(038) First published 1916 Fifth edition 1972 © Crown copyright 1972 Printed and published by HER MAJESTY'S STATIONERY OFFICE To be purchased from 49 High Holborn, London WC1V 6HB 13a Castle Street, Edinburgh EH2 3AR 109 St Mary Street, Cardiff CF1 1JW Brazennose Street, Manchester M60 8AS 50 Fairfax Street, Bristol BS1 3DE 258 Broad Street, Birmingham Bl 2HE 80 Chichester Street, Belfast BT1 4JY or through booksellers Price £2-75 net SBN 11 400208 8* PREFACE TO THE FIFTH EDITION When, in 1967, the Meteorological glossary came under consideration for reprinting, it was decided to ask Dr Mclntosh to undertake a revised edition, with co operation from within the Meteorological Office. The opportunity has been taken in this edition, to delete some terms which are considered no longer appropriate, and to include various new entries and revisions which stem from recent advances and practice. Units of the Systeme International have been adopted in this edition. In some cases, however, the traditional British or metric units are also included because of existing World Meteorological Organization recommendations and for the con venience of user interests during the period before complete national and inter national adoption of SI units. Meteorological Office, 1970. PREFACE TO THE FOURTH EDITION In 1916, during the directorship of Sir Napier Shaw, the Meteorological Office published two pocket-size companion volumes, the 'Weather map' to explain how weather maps were prepared and used by the forecasters, and the 'Meteorological glossary' to explain the technical meteorological terms then employed. -
Identification of Processes Driving Low-Level Westerlies in West
1JUNE 2014 P O K A M E T A L . 4245 Identification of Processes Driving Low-Level Westerlies in West Equatorial Africa WILFRIED M. POKAM Department of Physics, Higher Teacher Training College, University of Yaounde 1, and Center for International Forestry Research, Central Africa Regional Office, Yaounde, Cameroon CAROLINE L. BAIN,ROBIN S. CHADWICK, AND RICHARD GRAHAM Met Office Hadley Centre, Exeter, United Kingdom DENIS JEAN SONWA Center for International Forestry Research, Central Africa Regional Office, Yaounde, Cameroon FRANCOIS MKANKAM KAMGA University of Mountain, Bangangte, Cameroon (Manuscript received 8 August 2013, in final form 16 January 2014) ABSTRACT This paper investigates and characterizes the control mechanisms of the low-level circulation over west equatorial Africa (WEA) using four reanalysis datasets. Emphasis is placed on the contribution of the di- vergent and rotational circulation to the total flow. Additional focus is made on analyzing the zonal wind component, in order to gain insight into the processes that control the variability of the low-level westerlies (LLW) in the region. The results suggest that the control mechanisms differ north and south of 68N. In the north, the LLW are primarily a rotational flow forming part of the cyclonic circulation driven primarily by the heat low of the West African monsoon system. This northern branch of the LLW is well developed from June to August and disappears in December–February. South of 68N, the seasonal variability of the LLW is controlled by the heating contrast between cooling associated with subsidence over the ocean and heating over land regions largely south of the equator, where ascent prevails. -
SANGO 2019 Memo
SANGO 2019 Memo Correct answers are in red 1. Based on the population density map of China, it can be correctly inferred that: a. Western China is mountainous where subsistence agriculture is practiced. b. North-eastern China is a desert area dedicated to goat farming. c. Northern China is urbanized with significant industrial operations. d. Eastern China is dedicated to agricultural production on the floodplains. 2. Which of the four stages in the demographic transition model are considered “homeostatic” stages, that is, when the forces of demographic change are in equilibrium? a. Stages 1 and 3. b. Stage 3 and 4. c. Stages 2 and 3. d. Stages 1 and 4. 3. Which of the following strategies was identified by the 2004 United Nations International Conference on Population and Development as the most powerful approach for reducing the global population growth rate? a. Removing anti-contraception laws in conservative countries. b. Reducing vaccination rates. c. Empowering women in less-developed countries. d. Enforcing demographic growth rate targets. 4. At the centre of this relief map is the country of Iran. What type of landscape feature dominates the Iranian landscape? a. Floodplain. b. Plateau. c. Rift valley. d. Mesa. 5. The islands of the Pacific are home to some of the world’s first climate change refugees. This is primarily because of: a. Floods destroying agriculture. b. Tropical cyclones destroying infrastructure. c. Rising sea levels inundating habitable areas. d. Increasing ocean salinity causing fish die off. 6. The correct labels for the numbers 3, 6, 12, and 13 in this cross-section of a volcano are, in order: a.