Results 71 to 80 of about 22,988 (117)
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Climate Variability and Global Warming
Science, 2001Although uncertainties in global warming are many and varied, they are not as great as stated in the recent U.S. National Research Council (NRC) report ([1][1]). As Richard A. Kerr notes in his News of the Week article, President George W. Bush seized upon these uncertainties to justify the administration's limited response (“Bush backs spending for a ‘
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Climatic warming and the degradation of warm permafrost
Permafrost and Periglacial Processes, 1996Permafrost—a widespread constituent of the terrestrial environment—by definition is dependent upon the ambient temperature for its existence and properties. Thus, it is very sensitive to climatic changes. Simple relations based upon conductive heat transfer, with thawing and geothermal heat flow, are presented to predict the transient effects of ...
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2003
Most of the warm areas in the world lie between 0 to 34°N and S. Major potato production occurs between 23°N and 34°N and represents the subtropical lowlands, where potato is a winter crop (Hijmans, 2001). During the last three decades, potato areas increased in the developing world and North America while it decreased in Europe (FAO 2000, 2001).
S. M. Paul Khurana, I. D. Garg
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Most of the warm areas in the world lie between 0 to 34°N and S. Major potato production occurs between 23°N and 34°N and represents the subtropical lowlands, where potato is a winter crop (Hijmans, 2001). During the last three decades, potato areas increased in the developing world and North America while it decreased in Europe (FAO 2000, 2001).
S. M. Paul Khurana, I. D. Garg
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Global warming and climatic changes
2008Bu çalışmada, yeryüzündeki yaşamı tehdit eden küresel ısınma ve iklim değişikliği ile bu olayların etkileri ele alınmıştır. Son 100 yıl içerisinde yer yüzünde sıcaklığın 0.7-0.8 °C civarında arttığı tespit edilmiştir. Şayet gerekli önlemler alınmaz ise sıcaklık artışının artarak devam edeceği tahmin edilmektedir.
SAĞLAM, Naciye Erdoğan +2 more
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1986
Mainly because there are many overseas readers of this book but also because UK readers are increasingly requiring a knowledge of overseas building practice, it seemed desirable to add a further chapter describing the main problems experienced and the techniques used to overcome them.
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Mainly because there are many overseas readers of this book but also because UK readers are increasingly requiring a knowledge of overseas building practice, it seemed desirable to add a further chapter describing the main problems experienced and the techniques used to overcome them.
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2000
Pecan [Carya illinoensis (Wangenh. C. Koch)] production can be divided into two categories, production in dry and production in humid climates. Production in dry climates can be subdivided into production in low elevation climates and production in high elevation climates.
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Pecan [Carya illinoensis (Wangenh. C. Koch)] production can be divided into two categories, production in dry and production in humid climates. Production in dry climates can be subdivided into production in low elevation climates and production in high elevation climates.
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Science, 1996
The present climate, which falls between the last ice age and the next, is relatively stable. New data on past climate change, however, indicates that the climate is capable of undergoing abrupt changes from one mode to another. In his Perspective, Overpeck describes the current research into the history of climate change and how it might influence our
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The present climate, which falls between the last ice age and the next, is relatively stable. New data on past climate change, however, indicates that the climate is capable of undergoing abrupt changes from one mode to another. In his Perspective, Overpeck describes the current research into the history of climate change and how it might influence our
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Hurricanes in a warming climate
2013Changes in future Southern Hemisphere tropical cyclone numbers, by Kevin Walsh, Micahel Horn, Suzana Camargo, Hiroyuki Murakami, Hui Wang, and Enrico Scoccimarro; Tropcal cyclones in high-resolution climate models, by Suzana J. Camargo; Sensitivity of tropical cyclone simulation to SST forcing, by Malcolm Roberts, Pier Luigi Vidale, Ray Bell, and Kevin
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