Vegetation response to the ~14.7 and ~11.5 ka cal. BP climate transitions: is vegetation lagging climate?

By Hoek W.Z.  

Global and Planetary Change, Vol. 30, Iss. 1, 2001-09 ,pp. : 103-115

Elsevier

Access to resources Recommend Favorite

Simulation of the Younger Dryas climate in Europe using a regional climate model nested in an AGCM: preliminary results

By Renssen H.   Isarin R.F.B.   Jacob D.   Podzun R.   Vandenberghe J.  

Global and Planetary Change, Vol. 30, Iss. 1, 2001-09 ,pp. : 41-57

Elsevier

Access to resources Recommend Favorite

North Atlantic sea-surface temperature changes and the climate of western Iberia during the last deglaciation; a marine palynological approach

By Boessenkool K.P.   Brinkhuis H.   Schonfeld J.   Targarona J.  

Global and Planetary Change, Vol. 30, Iss. 1, 2001-09 ,pp. : 33-39

Elsevier

Access to resources Recommend Favorite

Variations in the influence of riverine discharge on the Kara Sea during the last deglaciation and the Holocene

By Polyak L.   Levitan M.   Khusid T.   Merklin L.   Mukhina V.  

Global and Planetary Change, Vol. 32, Iss. 4, 2002-04 ,pp. : 291-309

Elsevier

Access to resources Recommend Favorite

Press Release The Sun's Influence is an Important Factor in Global Climate Change – However, the rapid warming during the last 20 years is dominated by other factors

By  

Space Science Reviews, Vol. 94, Iss. 1-2, 2000-11 ,pp. : 423-424

Springer Publishing Company

Access to resources Recommend Favorite