Proceedings of the Royal Society of Victoria, Volumes 17-18

Royal Society Of Victoria (Melbourne, Vic.), .

Published by Ulan Press
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B00B06CHS6 Used good or better, we ship best copy available! May have signs of use, may be ex library copy. Book Only. Expedited shipping is 2-6 business days after shipment, standard is 4-14 business days after shipment. Used items do not include access codes, cd's or other accessories, regardless of what is stated in item title. If you need to guarantee that these items are included, please purchase a brand new copy. Bookseller Inventory #

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Title: Proceedings of the Royal Society of Victoria...
Publisher: Ulan Press


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Royal Society of Victoria
Published by Rarebooksclub.com, United States (2013)
ISBN 10: 1236928350 ISBN 13: 9781236928351
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Book Description Rarebooksclub.com, United States, 2013. Paperback. Book Condition: New. 246 x 189 mm. Language: English . Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1881 edition. Excerpt: . in the north the winds range from N.W. to N.E., and in the south from S.W. to S.E. This is the normal state of affairs in summer, and all around our coast sea breezes prevail. But now if one of the constantly recurring whirls or cyclonic movements of the atmosphere, forming perhaps at the Cape of Good Hope, or on the ocean between here and there, should approach our western or south-western coast, a change of affairs very soon becomes apparent. In Western Australia, or perhaps first at Cape Borda or Cape Northumberland, the barometer begins to fall, the wind coming from N.E., then increasing from north; then the barometers at Portland, Cape Otway, George Town, Melbourne, Wilson s Promontory, fall in succession with a northerly wind, which increases in force as the pressure gets less; this wind, blowing from an area of higher to an area of lower pressure, although still from around the summer low pressure area of Central Australia, comes down to us heated by the tropical sun, and by travelling over regions of heated earth s surface, producing the hot wind of South Australia and Victoria. These hot winds are always in front of cyclonic movements, and are fully explained by them. As the cyclonic area approaches, moving eastwards, the barometer still continues to fall, while the temperature increases. The question now arises, Where is the centre of this area, and where will it pass? The way the wind shifts tells us of this. So long as the wind is north, the centre is to the west of us; if it shifts from N. to N.W., as is most frequently the case here, the centre passes to the south of us; if it falls calm, with perhaps clear sky and very low barometer, the centre passes over us; but if the wind backs from N. to NE. and E., it. Bookseller Inventory # APC9781236928351

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Royal Society of Victoria
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Book Description RareBooksClub. Paperback. Book Condition: New. This item is printed on demand. Paperback. 100 pages. Dimensions: 9.7in. x 7.4in. x 0.2in.This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1881 edition. Excerpt: . . . in the north the winds range from N. W. to N. E. , and in the south from S. W. to S. E. This is the normal state of affairs in summer, and all around our coast sea breezes prevail. But now if one of the constantly recurring whirls or cyclonic movements of the atmosphere, forming perhaps at the Cape of Good Hope, or on the ocean between here and there, should approach our western or south-western coast, a change of affairs very soon becomes apparent. In Western Australia, or perhaps first at Cape Borda or Cape Northumberland, the barometer begins to fall, the wind coming from N. E. , then increasing from north; then the barometers at Portland, Cape Otway, George Town, Melbourne, Wilsons Promontory, fall in succession with a northerly wind, which increases in force as the pressure gets less; this wind, blowing from an area of higher to an area of lower pressure, although still from around the summer low pressure area of Central Australia, comes down to us heated by the tropical sun, and by travelling over regions of heated earths surface, producing the hot wind of South Australia and Victoria. These hot winds are always in front of cyclonic movements, and are fully explained by them. As the cyclonic area approaches, moving eastwards, the barometer still continues to fall, while the temperature increases. The question now arises, Where is the centre of this area, and where will it pass The way the wind shifts tells us of this. So long as the wind is north, the centre is to the west of us; if it shifts from N. to N. W. , as is most frequently the case here, the centre passes to the south of us; if it falls calm, with perhaps clear sky and very low barometer, the centre passes over us; but if the wind backs from N. to NE. and E. , it. . . This item ships from La Vergne,TN. Paperback. Bookseller Inventory # 9781236928351

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Royal Society of Victoria
Published by Rarebooksclub.com, United States (2013)
ISBN 10: 1236928350 ISBN 13: 9781236928351
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Book Description Rarebooksclub.com, United States, 2013. Paperback. Book Condition: New. 246 x 189 mm. Language: English . Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1881 edition. Excerpt: . in the north the winds range from N.W. to N.E., and in the south from S.W. to S.E. This is the normal state of affairs in summer, and all around our coast sea breezes prevail. But now if one of the constantly recurring whirls or cyclonic movements of the atmosphere, forming perhaps at the Cape of Good Hope, or on the ocean between here and there, should approach our western or south-western coast, a change of affairs very soon becomes apparent. In Western Australia, or perhaps first at Cape Borda or Cape Northumberland, the barometer begins to fall, the wind coming from N.E., then increasing from north; then the barometers at Portland, Cape Otway, George Town, Melbourne, Wilson s Promontory, fall in succession with a northerly wind, which increases in force as the pressure gets less; this wind, blowing from an area of higher to an area of lower pressure, although still from around the summer low pressure area of Central Australia, comes down to us heated by the tropical sun, and by travelling over regions of heated earth s surface, producing the hot wind of South Australia and Victoria. These hot winds are always in front of cyclonic movements, and are fully explained by them. As the cyclonic area approaches, moving eastwards, the barometer still continues to fall, while the temperature increases. The question now arises, Where is the centre of this area, and where will it pass? The way the wind shifts tells us of this. So long as the wind is north, the centre is to the west of us; if it shifts from N. to N.W., as is most frequently the case here, the centre passes to the south of us; if it falls calm, with perhaps clear sky and very low barometer, the centre passes over us; but if the wind backs from N. to NE. and E., it. Bookseller Inventory # APC9781236928351

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Royal Society of Victoria (Melbourne, Vi
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Book Description Palala Press, 2016. Paperback. Book Condition: New. PRINT ON DEMAND Book; New; Publication Year 2016; Not Signed; Fast Shipping from the UK. No. book. Bookseller Inventory # ria9781342857859_lsuk

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Royal Society of Victoria
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Book Description Arkose Press, 2015. HRD. Book Condition: New. New Book. Delivered from our US warehouse in 10 to 14 business days. THIS BOOK IS PRINTED ON DEMAND.Established seller since 2000. Bookseller Inventory # IP-9781345056594

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Royal Society of Victoria
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Book Description Palala Press, 2015. HRD. Book Condition: New. New Book. Delivered from our US warehouse in 10 to 14 business days. THIS BOOK IS PRINTED ON DEMAND.Established seller since 2000. Bookseller Inventory # IP-9781342857859

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Royal Society of Victoria
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Book Description Arkose Press, 2015. HRD. Book Condition: New. New Book. Delivered from our US warehouse in 10 to 14 business days. THIS BOOK IS PRINTED ON DEMAND.Established seller since 2000. Bookseller Inventory # IP-9781344938235

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Royal Society of Victoria (Melbourne, Vi
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Book Description Arkose Press, 2016. Paperback. Book Condition: New. PRINT ON DEMAND Book; New; Publication Year 2016; Not Signed; Fast Shipping from the UK. No. book. Bookseller Inventory # ria9781344938235_lsuk

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Royal Society Of Victoria (Melbourne, Vi
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Book Description Arkose Press, 2016. Paperback. Book Condition: New. PRINT ON DEMAND Book; New; Publication Year 2016; Not Signed; Fast Shipping from the UK. No. book. Bookseller Inventory # ria9781345056594_lsuk

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Book Description Arkose Press, United States, 2015. Hardback. Book Condition: New. 234 x 156 mm. Language: English . Brand New Book ***** Print on Demand *****. This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work.This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work.As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant. Bookseller Inventory # APC9781345056594

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