<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>13</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ball, Timothy</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">â€œAs cold as ever I knew it.â€ Joseph Colen, February 22nd, 1802. The Changing Climate of Manitoba</style></title></titles><dates><year><style  face="normal" font="default" size="100%">Submitted</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.mhs.mb.ca/docs/transactions/3/changingclimate.shtml</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">misc</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ball, Timothy F.</style></author><author><style face="normal" font="default" size="100%">Kingsley, Roger A.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Instrumental temperature records at two sites in Central Canada: 1768 to 1910</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1984</style></year><pub-dates><date><style  face="normal" font="default" size="100%">mar</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1007/BF00141667</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">6</style></volume><pages><style face="normal" font="default" size="100%">39-56</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">As a result of affiliation between the Hudson's Bay Company and the Royal Society a relatively large number of instrumental temperature records are available from York Factory and Churchill Factory on the southwest of Hudson Bay beginning in 1768. The nature of these records, details of the instruments and information about the observers are presented. The major difficulty with the records is that the number of observations and the time of observation varied considerably. Adjustment factors were calculated for all of the combinations using a modern record maintained at the Churchill airport. By combining the Hudson's Bay Company record with data recorded by members of the Royal Canadian Mounted Police after 1852, and up to 1910, a long and relatively continuous record of daily and monthly average temperatures has been created for Central Canada.</style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ball, Timothy</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A Dramatic Change in the General Circulation on the West Coast of Hudson Bay in 1760 AD: Synoptic Evidence Based on Historic Records</style></title><secondary-title><style face="normal" font="default" size="100%">Syllogeus</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1985</style></year></dates><volume><style face="normal" font="default" size="100%">55</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ball, Timothy</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Climate of Two Locations on the Southwestern Corner of Hudson Bay: A.D. 1720-1729</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Climatology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1994</style></year></dates><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ball, Timothy</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Preliminary Analysis of Early Instrumental Temperature Records from York Factory and Churchill Factory</style></title><secondary-title><style face="normal" font="default" size="100%">Syllogeus</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">Submitted</style></year></dates><volume><style face="normal" font="default" size="100%">49</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ball, Timothy</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The migration of geese as an indicator of climate change in the southern Hudson Bay region between 1715 and 1851</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1983</style></year><pub-dates><date><style  face="normal" font="default" size="100%">mar</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1007/BF02423429</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">5</style></volume><pages><style face="normal" font="default" size="100%">85-93</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Abstract  Observations and records maintained by the Hudson's Bay Company at York Factory and Churchill Factory on Hudson Bay between 1714 and 1825, serve as the source of information for a study of changes in the date of arrival of geese as a phonological indicator of climatic change. Changes in the migration pattern of geese are reflected in the changing date of arrival at the same location over a long period of time. Variations in this date are determined to be a function of southerly or tailwinds in the northward spring migration. </style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bradley, Raymond S.</style></author><author><style face="normal" font="default" size="100%">Jones, Philip D</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Climate Since A.D. 1500</style></title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Climatic changes</style></keyword><keyword><style  face="normal" font="default" size="100%">Paleoclimatology</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1992</style></year></dates><pub-location><style face="normal" font="default" size="100%">London ; New York</style></pub-location><isbn><style face="normal" font="default" size="100%">0415075939</style></isbn><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">book</style></work-type><notes><style face="normal" font="default" size="100%">Physical descrip: xv, 679 p. : ill., maps ; 26 cm
Bibliography note: Includes bibliographical references and index
Added title: Climate since AD 1500</style></notes></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Catchpole, A. J. W.</style></author><author><style face="normal" font="default" size="100%">Hanuta, Irene</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Severe summer ice in Hudson Strait and Hudson Bay following major volcanic eruptions, 1751 to 1889 A.D.</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1989</style></year><pub-dates><date><style  face="normal" font="default" size="100%">feb</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1007/BF00140175</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><pages><style face="normal" font="default" size="100%">61-79</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Indices of summer sea ice severity in the eighteenth and nineteenth centuries have been reconstructed from sailing ships' log-books. The ice record for Hudson Strait extends from 1751 to 1889. Ice records are available for two parts of Hudson Bay and these extend from 1751 to 1870. The three records were derived from the same sources but the method of derivation applied in the bay was different to that applied in the strait. The years having the five largest ice indices in each of these records were identified. Also identified were the years in which major volcanic eruptions occurred between 1751 and 1889. The number of concurrences between the years with severe ice in Hudson Strait and the years with major eruptions was significant at the 99.5\% level. In the western part of Hudson Bay this significance level was 95\%. The years with severe ice in eastern Hudson Bay did not concur with major eruptions.</style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Catchpole, A. J. W.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Historical Evidence of Climatic Change in Western and Northern Canada</style></title><secondary-title><style face="normal" font="default" size="100%">Syllogeus</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1980</style></year></dates><volume><style face="normal" font="default" size="100%">26</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Catchpole, A. J. W.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Ships' Log-books, Sea Ice and the Cold Summer of 1816 in Hudson Bay and Its Approaches</style></title><secondary-title><style face="normal" font="default" size="100%">Arctic</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1985</style></year></dates><volume><style face="normal" font="default" size="100%">38</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Catchpole, A. J. W.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Measuring Summer Sea Ice Severity in Eastern Hudson Bay, 1751-1870</style></title><secondary-title><style face="normal" font="default" size="100%">Canadian Geographer</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1987</style></year></dates><volume><style face="normal" font="default" size="100%">31</style></volume><pages><style face="normal" font="default" size="100%">233-244</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Catchpole, A.</style></author><author><style face="normal" font="default" size="100%">Faurer, Marcia-Anne</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Summer sea ice severity in Hudson Strait, 1751â€“1870</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1983</style></year><pub-dates><date><style  face="normal" font="default" size="100%">jun</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1007/BF02423486</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">5</style></volume><pages><style face="normal" font="default" size="100%">115-139</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Abstract  Annual indices of sea ice severity in Hudson Strait, for the period 1751 to 1870, are derived from written historical evidence contained in ships' log-books. These logs were all kept on Hudson's Bay Company ships sailing from London to the Company's trading posts. The log-books are homogeneous in nature and this property facilitates their numerical interpretation. The annual indices are subjected to face validity testing which indicates that they may plausibly be accepted as measures of sea ice severity. The results are examined in relation to the presentday behaviour of sea ice in Hudson Strait and they provide evidence that the summer severity of ice conditions is mainly determined by atmospheric circulation conditions. </style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Comeau, Martin</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Archives, historical climate records, and the climate observations of Thomas Corcoran, Hudson's Bay Company, 1827--1841</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><publisher><style face="normal" font="default" size="100%">University of Manitoba</style></publisher><pages><style face="normal" font="default" size="100%">105</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">phdthesis</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">D'Arrigo, Rosanne D.</style></author><author><style face="normal" font="default" size="100%">Jacoby, Gordon C.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Northern North American Tree-Ring Evidence for Regional Temperature Changes after Major Volcanic Events</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1023/A:1005370210796</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">41</style></volume><pages><style face="normal" font="default" size="100%">1-15</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Maximum latewood density data from trees at thirteen temperature-sensitive sites along the northern treeline of North America are used to evaluate the spatial patterns of response to four known volcanic events just prior to the period of modern observations: in 1640, 1783, 1815 and 1835. A previously unknown event is also postulated for 1699. This tree-ring density parameter is used because it shows a stronger and more consistent short-term, temperature-related volcanic signal than ring width. Normalized density departures following these events vary in sign and magnitude from region to region, with the coldest summer conditions inferred for the Northwest Territories in 1641, Alaska in 1783, Quebec and Labrador in 1816 and the Northwest Territories in 1836. For these as well as other events, low density values are often among the most extreme on record at their respective locations. We suggest that these regional variations in tree growth reflect cooling induced by volcanism and the distribution of cooling influenced by atmospheric circulation patterns.</style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Grumet, Nancy</style></author><author><style face="normal" font="default" size="100%">Wake, Cameron</style></author><author><style face="normal" font="default" size="100%">Mayewski, Paul</style></author><author><style face="normal" font="default" size="100%">Zielinski, Gregory</style></author><author><style face="normal" font="default" size="100%">Whitlow, Sallie</style></author><author><style face="normal" font="default" size="100%">Koerner, Roy</style></author><author><style face="normal" font="default" size="100%">Fisher, David</style></author><author><style face="normal" font="default" size="100%">Woollett, James</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Variability of Sea-Ice Extent in Baffin Bay over the Last Millennium</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2001</style></year><pub-dates><date><style  face="normal" font="default" size="100%">apr</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1023/A:1010794528219</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">49</style></volume><pages><style face="normal" font="default" size="100%">129-145</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Comparison of an ice core glaciochemical time-series developed from thePenny Ice Cap (PIC), Baffin Island and monthly sea-ice extent reveals astatisticallysignificant inverse relationship between changes in Baffin Bay spring sea-iceextent andPenny Ice Cap sea-salt concentrations for the period 1901â€“1990 AD.Empiricalorthogonal function analysis demonstrates the joint behavior between changesin PICsea-salt concentrations, sea-ice extent, and changes in North Atlanticatmosphericcirculation. Our results suggest that sea-salt concentrations in snowpreserved on thePIC reflect local to regional springtime sea-ice coverage. The PIC sea-saltrecord/sea-ice relationship is further supported by decadal and century scalecomparisonwith other paleoclimate records of eastern Arctic climate change over the last700 years. Our sea-salt record suggests that, while the turn of the century wascharacterized bygenerally milder sea-ice conditions in Baffin Bay, the last few decades ofsea-ice extentlie within Little Ice Age variability and correspond to instrumental recordsof lowertemperatures in the Eastern Canadian Arctic over the past three decades.</style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Harington, C. R. (Charles Richard)</style></author><author><style face="normal" font="default" size="100%">Rice, G.</style></author><author><style face="normal" font="default" size="100%">of Natural Sciences (Canada), National Museum</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Climatic Change in Canada: National Museum of Natural Sciences Project on Climatic Change in Canada During the Past 20,000 Years</style></title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Canada</style></keyword><keyword><style  face="normal" font="default" size="100%">Climatic changes</style></keyword><keyword><style  face="normal" font="default" size="100%">Climatology</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1980</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ottawa</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">book</style></work-type><notes><style face="normal" font="default" size="100%">Physical descrip: 5 v. : ill. ; 28 cm
Series: Syllogeus ; no. 26
Series: Syllogeus ; no. 33
Series: Syllogeus ; no. 49
Series: Syllogeus ; no. 51
Series: Syllogeus ; no. 55
General Note: Vol. 5 has subtitle: Critical periods in the quaternary climatic history of northern North America
General Note: Vol. 4 edited by C.R. Harington and G. Rice
Bibliography note: Includes bibliographical references
Local note: Alberta Geological Survey Library has no. 26, 49, 51, 55
Series: (Syllogeus,ISSN0704-576X ; no. 26, 33, 49, 51, 55)</style></notes></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Harington, C. R.</style></author><author><style face="normal" font="default" size="100%">of Nature, Canadian Museum</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Year Without a Summer?: World Climate in 1816</style></title></titles><keywords><keyword><style  face="normal" font="default" size="100%">1815</style></keyword><keyword><style  face="normal" font="default" size="100%">Case studies</style></keyword><keyword><style  face="normal" font="default" size="100%">Effect of volcanic eruptions on</style></keyword><keyword><style  face="normal" font="default" size="100%">Eruption</style></keyword><keyword><style  face="normal" font="default" size="100%">Mount (Indonesia)</style></keyword><keyword><style  face="normal" font="default" size="100%">Tambora</style></keyword><keyword><style  face="normal" font="default" size="100%">Weather</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1992</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ottawa</style></pub-location><isbn><style face="normal" font="default" size="100%">0660130637</style></isbn><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">book</style></work-type><notes><style face="normal" font="default" size="100%">Physical descrip: 576 p. : ill., maps ; 28 cm
Bibliography note: Includes bibliographical references and index
Summary: The objective of the meeting was, by bringing together workers in various fields (e.g., volcanologists, glaciologists, climatologists, tree-ring experts, geographers, historians and biologists) from various countries, to gain the clearest picture possible of weather and climatic sequences in different parts of the world during 1816, or about that time (e.g., 1810-20), in an effort to discover key factors influencing the unusual weather then.  Intended to discuss historical climate (particularly that of the Little Ice Age) and its human impact; relationships between volcanism and climate; and the ways paleoclimatic proxy data are gathered, treated and interpreted
Added title: World climate in 1816
Govt Canada class: NM95-20/1 1991-E</style></notes></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>13</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Moodie, D. W</style></author><author><style face="normal" font="default" size="100%">Catchpole, A. J. W.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Environmental Data from Historical Documents by Content Analysis: Freeze-up</style></title></titles><dates><year><style  face="normal" font="default" size="100%">1975</style></year></dates><publisher><style face="normal" font="default" size="100%">University of Manitoba, Department of Geography</style></publisher><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">misc</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rannie, W.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Breakup and freezeup of the Red River at Winnipeg, Manitoba Canada in the 19th century and some climatic implications</style></title><secondary-title><style face="normal" font="default" size="100%">Climatic Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1983</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1007/BF02423523</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">5</style></volume><pages><style face="normal" font="default" size="100%">283-296</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Abstract  Breakup and freezeup dates for the Red River at Winnipeg, Manitoba, Canada, were compiled from archival sources for the period from 1815 to the beginning of published data in 1908. Median 19th C dates of freezeup and break-up were 12 and 10 days earlier and later respectively than during the 20th C, and the average â€˜ice-inâ€™ season was nearly three weeks longer. Correlation of breakup and freezeup dates with spring and fall temperatures suggests that both seasons were about 25 C cooler in the 19th C than in the 20th. The change appears to have occurred rapidly at the end of the 19th C. </style></abstract><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slonosky, Victoria</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The meteorological observations of Jean-Francois Gaultier, Quebec, Canada: 1742-56</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Climate</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2003</style></year><pub-dates><date><style  face="normal" font="default" size="100%">jul</style></date></pub-dates></dates><volume><style face="normal" font="default" size="100%">16</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">article</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Teillet, John Vincent</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A reconstruction of summer sea ice conditions in the Labrador sea using Hudson's Bay Company ships' log-books, 1751 to 1870.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">1988</style></year></dates><publisher><style face="normal" font="default" size="100%">University of Manitoba</style></publisher><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">phdthesis</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>6</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Tompkins, Heather</style></author><author><style face="normal" font="default" size="100%">Queen's University (Kingston, Ont. )</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Historical Climatology of the Southern Yukon: Paleclimatic Reconstruction Using Documentary Sources from 1842-1852</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><publisher><style face="normal" font="default" size="100%">s.n.</style></publisher><pub-location><style face="normal" font="default" size="100%">Kingston, Ont</style></pub-location><isbn><style face="normal" font="default" size="100%">9780494154304</style></isbn><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">book</style></work-type></record><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Volek, John Vincent</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mid-winter thaws in the James Bay region, 1705-1992</style></title></titles><dates><year><style  face="normal" font="default" size="100%">1996</style></year></dates><publisher><style face="normal" font="default" size="100%">University of Manitoba</style></publisher><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">phdthesis</style></work-type></record></records></xml>
