De la rupture des glaces du Pôle Arctique

In the nineteenth century, scientists were convinced that the North Pole was free of ice. This myth was fostered since the eighteenth century, when it was thought that ice came from rivers and mainly formed near coasts. Rivers supposedly carried into the north seas a prodigious amount of glaçons or...

Full description

Bibliographic Details
Main Author: Aubriet, Antoine
Format: Book
Language:unknown
Published: Cambridge University Press 2012
Subjects:
Online Access:http://dx.doi.org/10.1017/cbo9781139225090
id crcambridgeupr:10.1017/cbo9781139225090
record_format openpolar
spelling crcambridgeupr:10.1017/cbo9781139225090 2024-03-03T08:42:01+00:00 De la rupture des glaces du Pôle Arctique Ou, observations géographiques, physiques et météorologiques sur les mers et les contrées du Pôle Arctique Aubriet, Antoine 2012 http://dx.doi.org/10.1017/cbo9781139225090 unknown Cambridge University Press https://www.cambridge.org/core/terms ISBN 9781108048279 9781139225090 monograph 2012 crcambridgeupr https://doi.org/10.1017/cbo9781139225090 2024-02-08T08:38:38Z In the nineteenth century, scientists were convinced that the North Pole was free of ice. This myth was fostered since the eighteenth century, when it was thought that ice came from rivers and mainly formed near coasts. Rivers supposedly carried into the north seas a prodigious amount of glaçons or 'ice cubes', which formed enormous masses of ice as they accumulated. This misconception led to an inaccurate climate theory that persisted until the beginning of the twentieth century: ice near a country's shores produces bitter cold in that country. This book, published in 1818, links the harsh winters of 1815–17 in England and Europe to the impressive amount of ice encountered at the same time in the Atlantic. The cold was thought to be caused by the break-up and southward drift of Arctic ice. It is attributed to the French meteorologist Antoine Aubriet, who was active in 1815–30. Book Arctic Arctique* North Pole Cambridge University Press Arctic North Pole Glaçons ENVELOPE(140.017,140.017,-66.659,-66.659) Cambridge
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language unknown
description In the nineteenth century, scientists were convinced that the North Pole was free of ice. This myth was fostered since the eighteenth century, when it was thought that ice came from rivers and mainly formed near coasts. Rivers supposedly carried into the north seas a prodigious amount of glaçons or 'ice cubes', which formed enormous masses of ice as they accumulated. This misconception led to an inaccurate climate theory that persisted until the beginning of the twentieth century: ice near a country's shores produces bitter cold in that country. This book, published in 1818, links the harsh winters of 1815–17 in England and Europe to the impressive amount of ice encountered at the same time in the Atlantic. The cold was thought to be caused by the break-up and southward drift of Arctic ice. It is attributed to the French meteorologist Antoine Aubriet, who was active in 1815–30.
format Book
author Aubriet, Antoine
spellingShingle Aubriet, Antoine
De la rupture des glaces du Pôle Arctique
author_facet Aubriet, Antoine
author_sort Aubriet, Antoine
title De la rupture des glaces du Pôle Arctique
title_short De la rupture des glaces du Pôle Arctique
title_full De la rupture des glaces du Pôle Arctique
title_fullStr De la rupture des glaces du Pôle Arctique
title_full_unstemmed De la rupture des glaces du Pôle Arctique
title_sort de la rupture des glaces du pôle arctique
publisher Cambridge University Press
publishDate 2012
url http://dx.doi.org/10.1017/cbo9781139225090
long_lat ENVELOPE(140.017,140.017,-66.659,-66.659)
geographic Arctic
North Pole
Glaçons
geographic_facet Arctic
North Pole
Glaçons
genre Arctic
Arctique*
North Pole
genre_facet Arctic
Arctique*
North Pole
op_source ISBN 9781108048279 9781139225090
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/cbo9781139225090
op_publisher_place Cambridge
_version_ 1792497526056681472