World Climates SECTION 2 If YOU Lived There
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January — March Year 2017
VOL 2 ISSUE 01 JANUARY — MARCH YEAR 2017 2016/17 DRY SEASON SUMMARY Dominica's dry season officially runs from December to May each year. The 2016 wet season, which prolonged into December resulting in a delay to the start of the 2016/17 dry season, was recorded as a normal season as it relates to rainfall amounts. A weak La Niña (the cooling of the Eastern Equatorial Pacific Ocean) was observed towards the end of 2016 and a transition to ENSO– neutral is expected during the period January to March 2017. La Niña tends to shift rainfall chances for January-February-March 2017 to above to normal in the southern-most is- lands of the Caribbean. With this occurrence, above to normal rainfall amounts are expected, resulting in less solar radiation and more cooling by clouds and more rainfall than last year. Temperatures are also expected to be closer to normal. IN THIS ISSUE Pg.1 2016/17 Dry-Season Dominica’s Climate Pg.2 Looking back at 2016 Pg.3 2016 Hurricane Season Looking ahead Pg.4 Seasonal Forecast Chart 1. Mid-December ENSO prediction plume DOMINICA’S CLIMATE Rainfall received during the dry season are usually generated by the annual migration of the North Atlantic Subtropical High, low level clouds which move with the easterly trade winds, southward dipping frontal boundaries and trough sys- tems. The dry season runs from December to May when the seas are cooler and thunderstorms and rainfall activity are relatively low. On average approximately 40% of the annual rainfall is recorded in elevated and eastern areas and ap- proximately 25% along the western coast. -
Weather Review and Outlook Towering Cumulus- Danny Gregoria by David Ross and Rob Molleda
Winter 2013 Welcome to this edition of Tropical Winds. Another hurricane season to be thankful for In This Issue… (…unless you are a hurricane junkie…). In Weather Review…………….….1 this edition, we will discuss what occurred Severe Weather Climo………...….7 during this year’s wet season and what to Hurricane Season 2013……………9 expect for the dry season. Also, we will talk about tornado climatology across South Employee Spotlight……………12 Florida. A look back at the 2013 Atlantic hurricane season will follow. To finish on a happy note, we will introduce you to another one of our devoted forecasters, Chris Duke. Happy Holidays!!! Weather Review and Outlook Towering Cumulus- Danny Gregoria By David Ross and Rob Molleda Looking Back at the Rainy Season May – October 2013 Synopsis The recently-concluded rainy season was wetter than normal across most of South Florida. It was very wet over most of southwest Florida where rainfall totals for the period from May 18th to October 10th (the duration of this year’s wet season) were in the 40 to 50 inch range, with a few spots exceeding 50 inches (Figure 1). This almost equals a year’s worth of rain in less than five months! Isolated spots in southeast Florida also recorded over 50 inches of rain, with most of this area receiving between 35 and 45 inches. Every month of the rainy season featured above normal rainfall over different parts of south Florida, with July being the wettest month overall due to a more widespread rainfall coverage, and August being the driest mostly across the eastern half of the peninsula (Figure 2). -
Canada GREENLAND 80°W
DO NOT EDIT--Changes must be made through “File info” CorrectionKey=NL-B Module 7 70°N 30°W 20°W 170°W 180° 70°N 160°W Canada GREENLAND 80°W 90°W 150°W 100°W (DENMARK) 120°W 140°W 110°W 60°W 130°W 70°W ARCTIC Essential Question OCEANDo Canada’s many regional differences strengthen or weaken the country? Alaska Baffin 160°W (UNITED STATES) Bay ic ct r le Y A c ir u C k o National capital n M R a 60°N Provincial capital . c k e Other cities n 150°W z 0 200 400 Miles i Iqaluit 60°N e 50°N R YUKON . 0 200 400 Kilometers Labrador Projection: Lambert Azimuthal TERRITORY NUNAVUT Equal-Area NORTHWEST Sea Whitehorse TERRITORIES Yellowknife NEWFOUNDLAND AND LABRADOR Hudson N A Bay ATLANTIC 140°W W E St. John’s OCEAN 40°W BRITISH H C 40°N COLUMBIA T QUEBEC HMH Middle School World Geography A MANITOBA 50°N ALBERTA K MS_SNLESE668737_059M_K.ai . S PRINCE EDWARD ISLAND R Edmonton A r Canada legend n N e a S chew E s kat Lake a as . Charlottetown r S R Winnipeg F Color Alts Vancouver Calgary ONTARIO Fredericton W S Island NOVA SCOTIA 50°WFirst proof: 3/20/17 Regina Halifax Vancouver Quebec . R 2nd proof: 4/6/17 e c Final: 4/12/17 Victoria Winnipeg Montreal n 130°W e NEW BRUNSWICK Lake r w Huron a Ottawa L PACIFIC . t S OCEAN Lake 60°W Superior Toronto Lake Lake Ontario UNITED STATES Lake Michigan Windsor 100°W Erie 90°W 40°N 80°W 70°W 120°W 110°W In this module, you will learn about Canada, our neighbor to the north, Explore ONLINE! including its history, diverse culture, and natural beauty and resources. -
Winds in the Lower Cloud Level on the Nightside of Venus from VIRTIS-M (Venus Express) 1.74 Μm Images
atmosphere Article Winds in the Lower Cloud Level on the Nightside of Venus from VIRTIS-M (Venus Express) 1.74 µm Images Dmitry A. Gorinov * , Ludmila V. Zasova, Igor V. Khatuntsev, Marina V. Patsaeva and Alexander V. Turin Space Research Institute, Russian Academy of Sciences, 117997 Moscow, Russia; [email protected] (L.V.Z.); [email protected] (I.V.K.); [email protected] (M.V.P.); [email protected] (A.V.T.) * Correspondence: [email protected] Abstract: The horizontal wind velocity vectors at the lower cloud layer were retrieved by tracking the displacement of cloud features using the 1.74 µm images of the full Visible and InfraRed Thermal Imaging Spectrometer (VIRTIS-M) dataset. This layer was found to be in a superrotation mode with a westward mean speed of 60–63 m s−1 in the latitude range of 0–60◦ S, with a 1–5 m s−1 westward deceleration across the nightside. Meridional motion is significantly weaker, at 0–2 m s−1; it is equatorward at latitudes higher than 20◦ S, and changes its direction to poleward in the equatorial region with a simultaneous increase of wind speed. It was assumed that higher levels of the atmosphere are traced in the equatorial region and a fragment of the poleward branch of the direct lower cloud Hadley cell is observed. The fragment of the equatorward branch reveals itself in the middle latitudes. A diurnal variation of the meridional wind speed was found, as east of 21 h local time, the direction changes from equatorward to poleward in latitudes lower than 20◦ S. -
How Important and Different Are Tropical Rivers? — an Overview
Geomorphology 227 (2014) 5–17 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph How important and different are tropical rivers? — An overview James P.M. Syvitski a,⁎,SagyCohenb,AlbertJ.Kettnera,G.RobertBrakenridgea a CSDMS/INSTAAR, U. of Colorado, Boulder, CO 80309-0545, United States b Dept. Geography, U. of Alabama, Tuscaloosa, AL 35487-0322, United States article info abstract Article history: Tropical river systems, wherein much of the drainage basin experiences tropical climate are strongly influenced Received 29 July 2013 by the annual and inter-annual variations of the Inter-tropical Convergence Zone (ITCZ) and its derivative mon- Received in revised form 19 February 2014 soonal winds. Rivers draining rainforests and those subjected to tropical monsoons typically demonstrate high Accepted 22 February 2014 runoff, but with notable exceptions. High rainfall intensities from burst weather events are common in the tro- Available online 11 March 2014 pics. The release of rain-forming aerosols also appears to uniquely increase regional rainfall, but its geomorphic Keywords: manifestation is hard to detect. Compared to other more temperate river systems, climate-driven tropical rivers Tropical climate do not appear to transport a disproportionate amount of particulate load to the world's oceans, and their warmer, Hydrology less viscous waters are less competent. Tropical biogeochemical environments do appear to influence the sedi- Sediment transport mentary environment. Multiple-year hydrographs reveal that seasonality is a dominant feature of most tropical rivers, but the rivers of Papua New Guinea are somewhat unique being less seasonally modulated. Modeled riverine suspended sediment flux through global catchments is used in conjunction with observational data for 35 tropical basins to highlight key basin scaling relationships. -
Contribution of Tropical Cyclones to Precipitation Around Reclaimed Islands in the South China Sea
water Article Contribution of Tropical Cyclones to Precipitation around Reclaimed Islands in the South China Sea Dongxu Yao 1,2, Xianfang Song 1,2,*, Lihu Yang 1,2,* and Ying Ma 1 1 Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; [email protected] (D.Y.); [email protected] (Y.M.) 2 Sino-Danish College, University of Chinese Academy of Sciences, Beijing 100049, China * Correspondence: [email protected] (X.S.); [email protected] (L.Y.); Tel.: +86-010-6488-9849 (X.S.); +86-010-6488-8266 (L.Y.) Received: 15 September 2020; Accepted: 2 November 2020; Published: 5 November 2020 Abstract: Tropical cyclones (TCs) play an important role in the precipitation of tropical oceans and islands. The temporal and spatial characteristics of precipitation have become more complex in recent years with climate change. Global warming tips the original water and energy balance in oceans and atmosphere, giving rise to extreme precipitation events. In this study, the monthly precipitation ratio method, spatial analysis, and correlation analysis were employed to detect variations in precipitation in the South China Sea (SCS). The results showed that the contribution of TCs was 5.9% to 10.1% in the rainy season and 7.9% to 16.8% in the dry season. The seven islands have the same annual variations in the precipitation contributed by TCs. An 800 km radius of interest was better for representing the contribution of TC-derived precipitation than a 500 km conventional radius around reclaimed islands in the SCS. -
Global Climate Influencer – Arctic Oscillation
ARCTIC OSCILLATION GLOBAL CLIMATE INFLUENCER by James Rohman | February 2014 Figure 1. A satellite image of the jet stream. Figure 2. How the jet stream/Arctic Oscillation might affect weather distribution in the Northern Hemisphere. Arctic Oscillation Introduction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
Globe Lesson 10 - Latitude Zones - Grade 6+ Geographers Divide the Earth Into Latitude Zones
Globe Lesson 10 - Latitude Zones - Grade 6+ Geographers divide the Earth into latitude zones. There are three latitude zones: - Low latitude zones - Middle latitude zones - High latitude zones There are 90 degrees of latitude. Each zone of latitude is 30 degrees wide. The Equator is 0 degrees. 0 to 30 are low numbers, 30-60 are middle numbers, and 60 to 90 are high numbers. This chart shows the arrangement of the zones in the Northern Hemisphere. Write in high, middle, and low latitude zones in the proper order in the Southern Hemisphere. Remember that the Equator is latitude 0 and the South Pole is latitude 90. Find the 180th meridian on your globe. On this line you will find the numbers of the printed parallels. Find 30 and 60 degrees north latitude. Draw a line of dashes around your globe on these lines. Find 30 and 60 degrees south latitude. Draw a line of dashes on these lines. These parallels divide the latitude zones. Label the zones Low, Middle and High in both the Northern and Southern Hemisphere on your globe. Finding Latitude Zones 4. In the following exercise identify the latitude with the proper latitude zone. "L" stands for low latitudes. "M" stands for middle latitudes. "H" stands for high latitudes. ______ 35°N ______ 23°N ______ 86°N ______ 15°N ______ 5°N ______ 66°N ______ 45°N ______ 28°N 5. In the following exercise, identify each city with the latitude zone where you find it. "L" stands for low latitudes. "M" stands for middle latitudes. -
Monthly Weather Review June1960
DEPARTMENT OF COMMERCE WEATHER BUREAU FREDERICK H. MUELLER, Secretary F. W.REICHELDERFER, Chief MONTHLYWEATHER REVIEW JAMESE. CASKEY, JR., Editor Volume 88 JUNE 1960 Closed August 15, 1960 Number 6 Issued September 15, 1960 THE SEASONAL VARIATION OF THE STRENGTH OF THE SOUTHERN CIRCUMPOLAR VORTEX W. SCHWERDTFEGER Department of Meteorology, Naval Hydrographic Service, Argentina [Manuscript received May 24, 1960; revised June 20, 19601 ABSTRACT The annual marchof the strengthof the southerncircumpolar. vortexis shown to be composed of a simple annual variation(with the maximumoccurring in late winter)which dominates in thestratosphere, and a semiannual variation with the maximum at the equinoxes, which is the dominating part in the troposphere. This behavior of the circumpolarvortex is considered to be the consequence of the seasonal variation of radiation conditions and of the different efficiency of meridional turbulent exchange in the troposphere and stratosphere. It is suggested that the semiannual variation of the tropospheric vortex is an essential feature of a planetary circulation. The annual march of pressure with opposite phase values at polar and middle latitudes, can be understood as a consequence of the formation and decay of the great circumpolar vortex. 1. INTRODUCTION part of the period which can now be considered. The Some aerological data of the Southern Hemisphere and South Pole station has been taken as representative of the particularly those from the South Pole (Amundsen-Scott inner part of the SCPV, in spiteof the fact that inseveral Station) obtained during theIGY and its extension through months the center of the vortex cannot be found exactly 1959, make it possible for the first time to arrive at an es- over the Pole. -
Climate and Vegetation • Almost Every Type of Climate Is Found in the 50 United States Because They Extend Over Such a Large Area North to South
123-126-Chapter5 10/16/02 10:16 AM Page 123 Main Ideas Climate and Vegetation • Almost every type of climate is found in the 50 United States because they extend over such a large area north to south. • Canada’s cold climate is related to its location in the far northern latitudes. A HUMAN PERSPECTIVE A little gold and bitter cold—that is what Places & Terms thousands of prospectors found in Alaska and the Yukon Territory dur- permafrost ing the Klondike gold rushes of the 1890s. Most of these fortune prevailing westerlies hunters were unprepared for the harsh climate and inhospitable land of Everglades the far north. Winters were long and cold, the ground frozen. Ice fogs, blizzards, and avalanches were regular occurrences. You could lose fin- Connect to the Issues gers and toes—even your life—in the cold. But hardy souls stuck it out. urban sprawl The rapid Legend has it that one miner, Bishop Stringer, kept himself alive by boil- spread of urban sprawl has led US & CANADA ing his sealskin and walrus-sole boots and then drinking the broth. to the loss of much vegetation in both the United States and Canada. Shared Climates and Vegetation The United States and Canada have more in common than just frigid winter temperatures where Alaska meets northwestern Canada. Other shared climate and vegetation zones are found along their joint border at the southern end of Canada and the northern end of the United States. If you look at the map on page 125, you will see that the United MOVEMENT The snowmobile States has more climate zones than Canada. -
Challenges in the Paleoclimatic Evolution of the Arctic and Subarctic Pacific Since the Last Glacial Period—The Sino–German
challenges Concept Paper Challenges in the Paleoclimatic Evolution of the Arctic and Subarctic Pacific since the Last Glacial Period—The Sino–German Pacific–Arctic Experiment (SiGePAX) Gerrit Lohmann 1,2,3,* , Lester Lembke-Jene 1 , Ralf Tiedemann 1,3,4, Xun Gong 1 , Patrick Scholz 1 , Jianjun Zou 5,6 and Xuefa Shi 5,6 1 Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung Bremerhaven, 27570 Bremerhaven, Germany; [email protected] (L.L.-J.); [email protected] (R.T.); [email protected] (X.G.); [email protected] (P.S.) 2 Department of Environmental Physics, University of Bremen, 28359 Bremen, Germany 3 MARUM Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany 4 Department of Geosciences, University of Bremen, 28359 Bremen, Germany 5 First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China; zoujianjun@fio.org.cn (J.Z.); xfshi@fio.org.cn (X.S.) 6 Pilot National Laboratory for Marine Science and Technology, Qingdao 266061, China * Correspondence: [email protected] Received: 24 December 2018; Accepted: 15 January 2019; Published: 24 January 2019 Abstract: Arctic and subarctic regions are sensitive to climate change and, reversely, provide dramatic feedbacks to the global climate. With a focus on discovering paleoclimate and paleoceanographic evolution in the Arctic and Northwest Pacific Oceans during the last 20,000 years, we proposed this German–Sino cooperation program according to the announcement “Federal Ministry of Education and Research (BMBF) of the Federal Republic of Germany for a German–Sino cooperation program in the marine and polar research”. Our proposed program integrates the advantages of the Arctic and Subarctic marine sediment studies in AWI (Alfred Wegener Institute) and FIO (First Institute of Oceanography). -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere.