DOCSLIB.ORG

+. 06 257 Weather of the Atlantic and Pacific Oceans

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
+. 06 257 Weather of the Atlantic and Pacific Oceans fun 1834 MONTHLY WEATHER REVIEW 257 WEATHER OF THE ATLANTIC AND PACIFIC OCEANS [The Marine Division, W.F. MCDONALDin charge] NORTH ATLANTIC OCEAN streamship lanes south and e.ast of Sable Island. The Gerinan moborship Ska,gerruk recorded force 12 on t,he By H. C. HUNTER forenoon of the 15th, near 40' N., GOo W., the only Atmospheric pressure.-The pressure during J~ly1934 instance of winds of hurricane force report,ed by any ship averaged reinarkably near normal in all pitrts of the during the w-hole niont81iin Atlnnt'ic waters. Later in the North Atlantic Ocean. Pressure was comparatively day the Ame,ricaii S.S. City of Hambwg and t,he French high during part of t8hefirst, decade over most northern liner Paris enc.ountered gales of force 11 at locations to sections, and the final decade was a period of rather high northeastwnrd of the Skagermk's positmion. The baro- pressure over middle and lower latitudes. On the 26th metric miniinurn of the Skagerruk, wt~28.94 inches, con- the French steamship Eliane L. D. noted a reading of siderably lower than :my other report received from t,he 30.72 inches near latitude 47' north, longitude 25' west, dt,lantic during July. (Chart VI11 present,s the weather the highest so far reported during the month. conditions on the 15t,li.) The following morning the st'orm was centered not far In general the lowest pressures occurred about the from Cape Ra.ce, and the intensity seeme.d considera.bly middle of the month. The lowest reading so far reported, diminished; nfter the morning of t'he 1Gt,h it no longer 28.94 inches, WRS observed on the 15th, by the German stood out dist,inctly as a feature of the weather situat,ion mo torship Skagerrak, as described below. over the At,lnntic. TABLE1.-Aoerages, depariurcs, and extremes of cdmospheric pres- The other notewort,hy storm may be recognized in siire (sea level) ai Sdec'led staiioirs juor the North dilartlic Oceun or111 developinent on the evening of t,he 21st, when pressure zts shores, Jiily 1934 was low at and near Savannah, Ga. This disturbance pursued an extraordinary course sout,liwest.\\..ardacross Average Depar- Highest Floricla into the Gulf. The progress at first was slow, Stations pressure ture the renter still being near Jaclisonville on the evening of ~~___the 2d,with intensity more marked bhan the day before ; Inches Inch Inrhrs Inchrs but, later move,nient was more rapid. When id1 out Julianehaab, Greenland_..__ 29.78 __._._..__30.00 2Y.49 I 10 Reykjavik, Iceland ......... 29.81) -0.04 30.07 268 1 29.35 31 from the coast, of the Gulf, t'he storm t,uriied to a west- Lerwick, Shetland Islands.. 3.90 +. 10 30.35 Valencia, Ireland___......_. 30.04 +. 06 30.40 ward course. Lisbon, Portugal___........ 30.01 -. 01 30.11 Madeira______._____........ 30.08 +.03 30. 17 The morning of t,he 35th found this storin ce,ntered Horta, Azores ...._......__._30.27 .OO 30. 5'2 not far enst of C,'orpus Christi, Tes., wit,h further increase Belle Isle, Newfoundland ... 29.80 -. 07 30. 13 Halifax, Nora Scotia........ 29.95 .OO 30.46 of ene,rgy (sea chart, IS). Therenft,er further westward Nantucket.___..__....._._._ 29.95 -.03 30.37 across 'Texas Hatteras_____.__.________._. 30.00 -.01 30.23 nioveinent, brought, t,he cent,er inland blie Bermuda ___..______________30.14 -.04 30.30 coast between Corpus Christi and Galveston, with high Turks Island _____._._...__.30.05 -.02 30.12 Key West 30.02 -.01 30.13 tide and dest,ructive winds. New Orleans 30.01 +.01 30.14 The lughest wind reported from the Gulf of Mexico during this storm was of force 10, noted a short distance NoTE.-A~~data based on a.m. observations only, with departures compiled from best available normals related to time of observation. except Hatteras, Key West. to nwtward of t,he 90t81imeridian during t,he afternoon Nantucket, and New Orleans, which are %-hour corrected means. of the 24t,h. No marine casualty of consequence ha.s come to notice as occurring on the ope,n Gulf because of Cyclones and gales.-To t,he nort,hward of the 44th this storm; but in Galveston Bay one steamship and a parallel a few vessels enc.ountered fresh gnles (force 8) barge were reported swept aground, t,liougli each was in different parts of the ocean on scatkerecl dates, but none later readily refloated. The effects of this storni on t>he of these gales was of general importance. For t,he ot,her coast and inla.nd are discussed elsewhere in this issue. portions of the Atlantic., interest is concentrated on two No storm whatever was reported froin the western well-marked storms. These were not felt, as far as ca.n Atlantic waters south of the Tropic of Cancer duiing be ascertained, anywhere south of the 25th parallel of the month. latitude; yet they exhibited many feat,ure,s c.haracteristic Fog.-There was considerably more fog over most of of the severe storms which often sta.rt in North Atlantic the North Atlantic steamship lanes between our north- tropical waters during the summer, and move thence in Lo ern ports and northwestern Europe t1ia.n there had been temperate waters. during June. As a result the amount during July was On the loth, there were signs of a small LOW, centered not far honi normal new mid-ocean, but usually a little not far eastward of Jac.ksonville, Fla. During the nest 3 less than normal in the eastern portion. On the Grand days moderate increase in energy, and gradual progress t,o Banks there WLS more fog than normal, notably in t,he northeastward were indicated, and during the la.te hours 5' square between 40' and 45' north, 45' and 50' west, of the 13th, 2 vessels bound from New York to Puerto diere fog w.ns noted during 25 days, including every Rico met fresh to whole gales in latitude about 33' nort,h, da,y save one from the 1lt)ht,o the last dn.y of the month, longitude 71' west. During the 14th, moderately strong inclusive. southerly winds prevailed at Bermuda. In the waters adjacent to the North and Middle The storm continued to northeastward and became the Atlantic States fog during July 1934 was less prevalent southeastward prolongation of a large LOW area that t(1ian it had been during the preceding month, and for extended over regions adjacent to Hudson Bay. On the the most part was a little less frequent than is normally 15th, winds of great strength were noted on the chief the case during July. Unauthenticated | Downloaded 09/28/21 04:25 PM UTC.
Load more

Recommended publications
  • IOM Regional Strategy 2020-2024 South America
    SOUTH AMERICA REGIONAL STRATEGY 2020–2024 IOM is committed to the principle that humane and orderly migration benefits migrants and society. As an intergovernmental organization, IOM acts with its partners in the international community to: assist in meeting the operational challenges of migration; advance understanding of migration issues; encourage social and economic development through migration; and uphold the human dignity and well-being of migrants. Publisher: International Organization for Migration Av. Santa Fe 1460, 5th floor C1060ABN Buenos Aires Argentina Tel.: +54 11 4813 3330 Email: [email protected] Website: https://robuenosaires.iom.int/ Cover photo: A Syrian family – beneficiaries of the “Syria Programme” – is welcomed by IOM staff at the Ezeiza International Airport in Buenos Aires. © IOM 2018 _____________________________________________ ISBN 978-92-9068-886-0 (PDF) © 2020 International Organization for Migration (IOM) _____________________________________________ All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise without the prior written permission of the publisher. PUB2020/054/EL SOUTH AMERICA REGIONAL STRATEGY 2020–2024 FOREWORD In November 2019, the IOM Strategic Vision was presented to Member States. It reflects the Organization’s view of how it will need to develop over a five-year period, in order to effectively address complex challenges and seize the many opportunities migration offers to both migrants and society. It responds to new and emerging responsibilities – including membership in the United Nations and coordination of the United Nations Network on Migration – as we enter the Decade of Action to achieve the Sustainable Development Goals.
    [Show full text]
  • North America Other Continents
    Arctic Ocean Europe North Asia America Atlantic Ocean Pacific Ocean Africa Pacific Ocean South Indian America Ocean Oceania Southern Ocean Antarctica LAND & WATER • The surface of the Earth is covered by approximately 71% water and 29% land. • It contains 7 continents and 5 oceans. Land Water EARTH’S HEMISPHERES • The planet Earth can be divided into four different sections or hemispheres. The Equator is an imaginary horizontal line (latitude) that divides the earth into the Northern and Southern hemispheres, while the Prime Meridian is the imaginary vertical line (longitude) that divides the earth into the Eastern and Western hemispheres. • North America, Earth’s 3rd largest continent, includes 23 countries. It contains Bermuda, Canada, Mexico, the United States of America, all Caribbean and Central America countries, as well as Greenland, which is the world’s largest island. North West East LOCATION South • The continent of North America is located in both the Northern and Western hemispheres. It is surrounded by the Arctic Ocean in the north, by the Atlantic Ocean in the east, and by the Pacific Ocean in the west. • It measures 24,256,000 sq. km and takes up a little more than 16% of the land on Earth. North America 16% Other Continents 84% • North America has an approximate population of almost 529 million people, which is about 8% of the World’s total population. 92% 8% North America Other Continents • The Atlantic Ocean is the second largest of Earth’s Oceans. It covers about 15% of the Earth’s total surface area and approximately 21% of its water surface area.
    [Show full text]
  • The Civil War Differences Between the North and South Geography of The
    Differences Between the North and The Civil War South Geography of the North Geography of the South • Climate – frozen winters; hot/humid summers • Climate – mild winters; long, hot, humid summers • Natural features: • Natural features: − coastline: bays and harbors – fishermen, − coastline: swamps and shipbuilding (i.e. Boston) marshes (rice & sugarcane, − inland: rocky soil – farming hard; turned fishing) to trade and crafts (timber for − inland: indigo, tobacco, & shipbuilding) corn − Towns follow rivers inland! Economy of the North Economy of the South • MORE Cities & Factories • Agriculture: Plantations and Slaves • Industrial Revolution: Introduction of the Machine − White Southerners made − products were made cheaper and faster living off the land − shift from skilled crafts people to less skilled − Cotton Kingdom – Eli laborers Whitney − Economy BOOST!!! •cotton made slavery more important •cotton spread west, so slavery increases 1 Transportation of the North Transportation of the South • National Road – better roads; inexpensive way • WATER! Southern rivers made water travel to deliver products easy and cheap (i.e. Mississippi) • Ships & Canals – river travels fast; steamboat • Southern town sprang up along waterways (i.e. Erie Canal) • Railroad – steam-powered machine (fastest transportation and travels across land ) Society of the North – industrial, urban Society of the South – life agrarian, rural life • Maine to Iowa • Black Northerners − free but not equal (i.e. segregation) • Maryland to Florida & west to Texas − worked
    [Show full text]
  • SOUTH AMERICA July/August 2007 GGETTINGETTING SSTARTEDTARTED: Guide
    SOUTH AMERICA July/August 2007 GGETTINGETTING SSTARTEDTARTED: Guide Is It Time for a ® South American Strategy? Localization Outsourcing ® and Export in Brazil Doing Business ® in Argentina The Tricky Business ® of Spanish Translation Training Translators ® in South America 0011 GGuideuide SSoAmerica.inddoAmerica.indd 1 66/27/07/27/07 44:13:40:13:40 PPMM SOUTH AMERICA Guide: GGETTINGETTING SSTARTEDTARTED Getting Started: Have you seen the maps where the Southern Hemisphere is at South America the top? “South-up” maps quite often are — incorrectly — referred to as “upside-down,” and it’s easy to be captivated by them. They Editor-in-Chief, Publisher Donna Parrish remind us in the Northern Hemisphere how region-centric we are. Managing Editor Laurel Wagers In this Guide to South America, we focus on doing business and work in Translation Department Editor Jim Healey South America. Greg Churilov and Florencia Paolillo address common trans- Copy Editor Cecilia Spence News Kendra Gray lation misconceptions in dealing with Spanish in South America. Jorgelina Illustrator Doug Jones Vacchino, Nicolás Bravo and Eugenia Conti describe how South American Production Sandy Compton translators are trained. Charles Campbell looks at companies that have Editorial Board entered the South American market with different degrees of success. Jeff Allen, Julieta Coirini, Teddy Bengtsson recounts setting up a company in Argentina. And Bill Hall, Aki Ito, Nancy A. Locke, Fabiano Cid explores Brazil, both as an outsourcing option and an Ultan Ó Broin, Angelika
    [Show full text]
  • 100 the SOUTH-WEST CORNER of QUEENSLAND. (By S
    100 THE SOUTH-WEST CORNER OF QUEENSLAND. (By S. E. PEARSON). (Read at a meeting of the Historical Society of Queensland, August 27, 1937). On a clear day, looking westward across the channels of the Mulligan River from the gravelly tableland behind Annandale Homestead, in south­ western Queensland, one may discern a long low line of drift-top sandhills. Round more than half the skyline the rim of earth may be likened to the ocean. There is no break in any part of the horizon; not a landmark, not a tree. Should anyone chance to stand on those gravelly rises when the sun was peeping above the eastem skyline they would witness a scene that would carry the mind at once to the far-flung horizons of the Sahara. In the sunrise that western region is overhung by rose-tinted haze, and in the valleys lie the purple shadows that are peculiar to the waste places of the earth. Those naked, drift- top sanddunes beyond the Mulligan mark the limit of human occupation. Washed crimson by the rising sun they are set Kke gleaming fangs in the desert's jaws. The Explorers. The first white men to penetrate that line of sand- dunes, in south-western Queensland, were Captain Charles Sturt and his party, in September, 1845. They had crossed the stony country that lies between the Cooper and the Diamantina—afterwards known as Sturt's Stony Desert; and afterwards, by the way, occupied in 1880, as fair cattle-grazing country, by the Broad brothers of Sydney (Andrew and James) under the run name of Goyder's Lagoon—and the ex­ plorers actually crossed the latter watercourse with­ out knowing it to be a river, for in that vicinity Sturt describes it as "a great earthy plain." For forty miles one meets with black, sundried soil and dismal wilted polygonum bushes in a dry season, and forty miles of hock-deep mud, water, and flowering swamp-plants in a wet one.
    [Show full text]
  • Coriolis Effect
    Project ATMOSPHERE This guide is one of a series produced by Project ATMOSPHERE, an initiative of the American Meteorological Society. Project ATMOSPHERE has created and trained a network of resource agents who provide nationwide leadership in precollege atmospheric environment education. To support these agents in their teacher training, Project ATMOSPHERE develops and produces teacher’s guides and other educational materials. For further information, and additional background on the American Meteorological Society’s Education Program, please contact: American Meteorological Society Education Program 1200 New York Ave., NW, Ste. 500 Washington, DC 20005-3928 www.ametsoc.org/amsedu This material is based upon work initially supported by the National Science Foundation under Grant No. TPE-9340055. Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the authors and do not necessarily reflect the views of the National Science Foundation. © 2012 American Meteorological Society (Permission is hereby granted for the reproduction of materials contained in this publication for non-commercial use in schools on the condition their source is acknowledged.) 2 Foreword This guide has been prepared to introduce fundamental understandings about the guide topic. This guide is organized as follows: Introduction This is a narrative summary of background information to introduce the topic. Basic Understandings Basic understandings are statements of principles, concepts, and information. The basic understandings represent material to be mastered by the learner, and can be especially helpful in devising learning activities in writing learning objectives and test items. They are numbered so they can be keyed with activities, objectives and test items. Activities These are related investigations.
    [Show full text]
  • Living and Working at USAP Facilities
    Chapter 6: Living and Working at USAP Facilities CHAPTER 6: Living and Working at USAP Facilities McMurdo Station is the largest station in Antarctica and the southermost point to which a ship can sail. This photo faces south, with sea ice in front of the station, Observation Hill to the left (with White Island behind it), Minna Bluff and Black Island in the distance to the right, and the McMurdo Ice Shelf in between. Photo by Elaine Hood. USAP participants are required to put safety and environmental protection first while living and working in Antarctica. Extra individual responsibility for personal behavior is also expected. This chapter contains general information that applies to all Antarctic locations, as well as information specific to each station and research vessel. WORK REQUIREMENT At Antarctic stations and field camps, the work week is 54 hours (nine hours per day, Monday through Saturday). Aboard the research vessels, the work week is 84 hours (12 hours per day, Monday through Sunday). At times, everyone may be expected to work more hours, assist others in the performance of their duties, and/or assume community-related job responsibilities, such as washing dishes or cleaning the bathrooms. Due to the challenges of working in Antarctica, no guarantee can be made regarding the duties, location, or duration of work. The objective is to support science, maintain the station, and ensure the well-being of all station personnel. SAFETY The USAP is committed to safe work practices and safe work environments. There is no operation, activity, or research worth the loss of life or limb, no matter how important the future discovery may be, and all proactive safety measures shall be taken to ensure the protection of participants.
    [Show full text]
  • Health in South America
    Health in South America 2012 Edition Health Situation, Policies and Systems Overview Health in South America 2012 Edition Health Situation, Policies and Systems Overview PAHO/WHO technical team that prepared the document: Principal authors and coordination: César Gattini and Patricia Ruiz. Contributors: Celia Riera, Elisabeth Duarte, Mariela Licha Salomón, Alejandro Gherardi, Fernando Llanos, Humberto Montiel, Rolando Ramírez, Félix Rígoli and Javier Uribe. Translation to English version: Catalina Palma (CONYCIT) Editorial review to English version: Daniela Gattini Health Information and Analysis Project (HSD/HA) Country Focus Support Office (CFS) Pan American Health Organization World Health Organization Washington DC, 2012 HEALTH IN SOUTH AMERICA, 2012 It is also published in Spanish: Salud en Sudamérica, edición de 2012: panorama de la situación de salud y de las políticas y sistemas de salud PAHO/WHO Headquarters Library - Cataloguing Pan American Health Organization Health in South America, 2012 Edition: Health Situation, Policies and Systems Overview Washington DC: 2012 ISBN: 978-92-75-31714-3 1. Health indicators 2. Health profile 3. Health inequities 4. Environmental health 5. Public policies 6. Health Systems and Services 7. South America The Pan American Health Organization will give consideration to requests for permission to reproduce or translate, in part or in full, any of its publications. Applications and inquiries should be addressed to Knowledge Management and Communication Area, Pan American Health Organization (PAHO), Washington, DC, United States of America ([email protected]). The Knowledge and Information Centre, Office of the PAHO / WHO Representation in Chile, Santiago, Chile, will provide information on any changes made to the text, plans for new editions, and reprints and translations already available.
    [Show full text]
  • Latitude/Longitude of the Exact Opposite Place LONGITUDE on Earth to Sydney, Australia, 33° 55‘ S, 151° 17‘ E 90° N 180° Sydney LATITUDE 151° 17’ E
    GEO 101, January 16, 2014, Latitude and Longitude Finding your way … How geographers locate where things are… Most common locational system Best reference points are ends of rotational axis Latitude and Longitude Measures angular distance in degrees, not distance in miles or km Basic geometry: circle has 360 degrees Babylonians (≈600 BC) chose the number 360. The reason is that their number system was based on 60. To compare, we base our number system on 10. For us, 10 is a nice, round number and we find it very convenient to count in multiples of 10. But the Babylonians liked 60. LATITUDE Midway between N & S pole is Equator = 0° 90° N 0° 90° S 1 Latitude of Mobile ≈ 30° 42’ N. Parallels of latitude measure the angular distance (degrees) north or south of the Equator. Expressed in degrees, minutes, & seconds 60 minutes in 1 degree 60 seconds in 1 minute The lines themselves run east - west like the rungs on a ladder Find distance in miles between Latitude can be used to approximate Mobile and the Galapagos Islands, distances based on following: which is almost due south of Mobile 360° in a circle Galapagos 0° 10’ S Mobile 30° 42’ N ≈ 25,000 miles around earth 25,000 miles / 360° ≈ 69 miles in 1° Difference 30° 52’ or 30 + 52/60 degrees = 30.87° One degree of latitude always ≈ 69 miles This is true because parallels of latitude 30.87° x 69 mi/degree = 2130 miles stay same distance apart LONGITUDE Arbitrary starting place at Greenwich (London), England 180° = International Date Line East West N P 0° = Prime Meridian 2 One degree of longitude ONLY EQUALS 69 Meridians of longitude measure the miles, at the Equator.
    [Show full text]
  • PRIME MERIDIAN a Place Is
    Lines of Latitude and Longitude help us to answer a key geographical question: “Where am I?” What are Lines of Latitude and Longitude? Lines of Latitude and Longitude refer to the grid system of imaginary lines you will find on a map or globe. PARALLELS of Latitude and MERIDIANS of Longitude form an invisible grid over the earth’s surface and assist in pinpointing any location on Earth with great accuracy; everywhere has its own unique grid location, and this is expressed in terms of LATITUDE and LONGITUDE COORDINATES. Lines of LATITUDE are the ‘horizontal’ lines. They tell us whether a place is located in the NORTHERN or the SOUTHERN HEMISPHERE as well as how far North or South from the EQUATOR it is. Lines of LONGITUDE are the ‘vertical’ lines. They indicate how far East or West of the PRIME MERIDIAN a place is. • The EQUATOR is the 0° LATITUDE LINE. o North of the EQUATOR is the NORTHERN HEMISPHERE. o South of the EQUATOR is the SOUTHERN HEMISPHERE. • Lines of Latitude cross the PRIME MERIDIAN (longitude line) at right angles (90°). • Lines of Latitude circle the globe/world in an east- west direction. • Lines of Latitude are also known as PARALLELS. o As they are parallel to the Equator and apart always at the same distance. • Lines of Latitude measure distance north or south from the equator i.e. how far north or south a point lies from the Equator. • The distance between degree lines is about 69 miles (or about 110km). o A DEGREE (°) equals 60 minutes - 60’.
    [Show full text]
  • South America: Human Geography
    R E S O U R C E L I B R A R Y E N C Y C L O P E D I C E N T RY South America: Human Geography Encyclopedic entry. South America’s human landscape is deeply influenced by indigenous and immigrant populations, and their connection to the physical environment. G R A D E S 6 - 12+ S U B J E C T S Arts and Music, Geography, Human Geography, Social Studies, World History C O N T E N T S 9 Images For the complete encyclopedic entry with media resources, visit: http://www.nationalgeographic.org/encyclopedia/south-america-human-geography/ South America, the fourth-largest continent, extends from the Gulf of Darién in the northwest to the Tierra del Fuego archipelago in the south. Along with the islands of Tierra del Fuego, the continent includes the Galápagos Islands (Ecuador), Easter Island (Chile), the Falkland Islands (United Kingdom), and the Chiloé and Juan Fernández archipelagos (Chile). South America and North America are named after Italian navigator Amerigo Vespucci, who was the first European to suggest that the Americas were not part of the East Indies, but an entirely separate landmass. The portions of the landmass that lie south of the Isthmus of Panama became known as South America. Today, South America is home to the citizens of Colombia, Venezuela, Guyana, Suriname, French Guiana, Brazil, Uruguay, Argentina, the Falkland Islands, Chile, Peru, Ecuador, Bolivia, and Paraguay. South America’s physical geography, environment and resources, and human geography can be considered separately.
    [Show full text]
  • The Greek Winds
    The Classical Review http://journals.cambridge.org/CAR Additional services for The Classical Review: Email alerts: Click here Subscriptions: Click here Commercial reprints: Click here Terms of use : Click here The Greek Winds D'Arcy Wentworth Thompson The Classical Review / Volume 32 / Issue 3-4 / May 1918, pp 49 - 56 DOI: 10.1017/S0009840X00011276, Published online: 27 October 2009 Link to this article: http://journals.cambridge.org/abstract_S0009840X00011276 How to cite this article: D'Arcy Wentworth Thompson (1918). The Greek Winds. The Classical Review, 32, pp 49-56 doi:10.1017/S0009840X00011276 Request Permissions : Click here Downloaded from http://journals.cambridge.org/CAR, IP address: 130.179.16.201 on 16 Feb 2015 The Review MAY—JUNE, 1918 ORIGINAL CONTRIBUTIONS THE GREEK WINDS. IN the orientation ot the Greek Caecias, Eurus, Lips, and Argestes Winds—that is to say, in the interpre- (Z, A, F, E) are (on this interpretation) tation of the Greek ' wind-rose,' or set midway between the four cardinal compass - card — there lies a pretty problem, which to my thinking is but little understood by scholars. The sub- K ject has been touched on of late by Sir Arthur Hort in his translation of Theo- phrastus De Signis, and by Mr. E. S. Forster in his Oxford translation of the Ps. Aristotelian Ventorum Situs et Appel- lationes. Both writers borrow their statements and their diagrams from W. Capelle's paper on the treatise De Mundo ('Die Schrift von der Welt,' Neue Jahrb. xv. 1905), as Capelle in turn had followed for the most part in the steps of Kaibel ('Antike Windrosen,' Hermes, xx.
    [Show full text]