Titlebook: History and Climate; Memories of the Futu P. D. Jones,A. E. J. Ogilvie,K. R. Briffa Book 2001 Springer Science+Business Media New York 2001

HARDY

书目名称History and Climate影响因子(影响力)




书目名称History and Climate影响因子(影响力)学科排名




书目名称History and Climate网络公开度




书目名称History and Climate网络公开度学科排名




书目名称History and Climate被引频次




书目名称History and Climate被引频次学科排名




书目名称History and Climate年度引用




书目名称History and Climate年度引用学科排名




书目名称History and Climate读者反馈




书目名称History and Climate读者反馈学科排名

钉牢

Pre-Instrumental Weather Observations in Poland in the 16th and 17th Centuriestion of the MWE occurred in the 12. and 13. centuries in the period 1150-1300 (Lamb, 1982). This warm period was followed by a colder one which lasted to the second half of the 19. century and is known as the so-called Little Ice Age (LIA). The climate during the LIA was not constantly cold. The rec

PHONE

诗集

Early European Instrumental Recordswever, have series been developed for the entire length of available data. The earliest measurements are unlikely to be consistent with today’s readings for a variety of reasons. Potential problems relate to uncertainties in the accuracy of the instrumentation, the units used, exposure, observation

集合

Circulation Changes in Europe since the 1780sll as effects of the former (Hupfer, 1991). Therefore, climate research should always include investigations on the behaviour of the circulation. This is valid within an historical perspective. In view of possible changes in climate that might be expected in the near future due to anthropogenic gree

tangle

A Millennium of Weather, Winds and Water in the Low Countriesresent-day Benelux) for the period 1000 to present is depicted and classified. In the books., the course of the weather during both the winter and summer season as well is followed from year to year and placed in a historical context. In summer 2000, Vol. IV, covering the era 1575–1700, will appear,

饰带

Long Climatic series from Austriaoject ALOCLIM (Austrian Long Term Climate) a homogenised data set, consisting of 274 single series (see Table 2) has been developed. In addition, results from previous investigations increase the number of homogenised time series to 350. However, it is not possible to describe the complicated climat

BRIDE

生命

Sea Ice-Climate-Glacier Relationships in Northern Iceland since the Nineteenth Century: Possible Anaigations presented in this paper. Iceland lies within the atmospheric and oceanic circulation of the North Atlantic. This determines the surrounding climatic and sea-ice conditions which, in turn, act upon indicators of the environmental system. Glacier behaviour (advance, standstill or retreat) is

META