Parámetros
- 353 páginas
- 13 horas de lectura
Más información sobre el libro
Some 115 thousand years ago the world as we know it todayshifted into a much colder glacial mode which culminatedwith huge ice sheets reaching as far south as New York,Berlin and St. Petersburg. The numerical climate models,used to predict the next century climate, were as yet unableto explain what happened.The reader of the book gains a detailed picture of what isknown on the most important episodes of the past climatehistory, what to expect during the transition into aglacial climate mode, and which aspects and elements of theclimate system seem mostsusceptible to change. The climatemodelers will realize that the long term history of naturalclimate variations may hold important clues to the mechanismof climate changes which should be taken in account if thenear future CO2 rich climate have to be predicted with anydegree ofreliability.
Compra de libros
NATO ASI Series, Series I: Global Environmental Change - 3: Start of a Glacial, George J. Kukla, Ellen Went
- Idioma
- Publicado en
- 1992
- product-detail.submit-box.info.binding
- (Tapa dura),
- Estado del libro
- Bueno
- Precio
- 7,49 €
Métodos de pago
Nadie lo ha calificado todavía.
- Título
- NATO ASI Series, Series I: Global Environmental Change - 3: Start of a Glacial
- Subtítulo
- Proceedings of the NATO Advanced Research Workshop on Correlating Records of the Past Held at Cabo Blanco, Mallorca, Spain, April 4–10, 1991
- Idioma
- Inglés
- Autores
- George J. Kukla, Ellen Went
- Editorial
- Springer
- Publicado en
- 1992
- Formato
- Tapa dura
- Páginas
- 353
- ISBN10
- 3540545859
- ISBN13
- 9783540545859
- Serie
- Etiquetas
- No ficción, Tema histórico, Historia, Ciencia y Matemáticas, Ciencias naturales, Ciencia, Temática ecológica, Ecología, Historia de la vida cotidiana, Cambio climático, Ciencias ambientales
- Descripción
- Some 115 thousand years ago the world as we know it todayshifted into a much colder glacial mode which culminatedwith huge ice sheets reaching as far south as New York,Berlin and St. Petersburg. The numerical climate models,used to predict the next century climate, were as yet unableto explain what happened.The reader of the book gains a detailed picture of what isknown on the most important episodes of the past climatehistory, what to expect during the transition into aglacial climate mode, and which aspects and elements of theclimate system seem mostsusceptible to change. The climatemodelers will realize that the long term history of naturalclimate variations may hold important clues to the mechanismof climate changes which should be taken in account if thenear future CO2 rich climate have to be predicted with anydegree ofreliability.