Past global climate changes had strong regional expression. To elucidate their spatio-
temporal pattern, we reconstructed past temperatures for seven continental-scale regions …

Canadian boreal woodlands and forests cover approximately 3.09× 106 km2, located within
a larger boreal zone characterized by cool summers and long cold winters. Warming since …

This chapter assesses the causes of observed changes assessed in Chapters 2 to 5 and
uses understanding of physical processes, climate models and statistical approaches. The …

Climate Variability and Change since 850 CE: An Ensemble Approach with the Community
Earth System Model in: Bulletin of the American Meteorological Society Volume 97 Issue 5 (2016) …

Abstract The United Nations Framework Convention on Climate Change (UNFCCC) process
agreed in Paris to limit global surface temperature rise to “well below 2° C above pre …

The present interglacial, the Holocene, spans the period of the last 11,700 years. It has
sustained the growth and development of modern society. The millennial-scale decreasing …

Climate change is the single most important global environmental and development issue
facing the world today and has emerged as a major topic in tourism studies. Climate change …

The Arctic is warming faster than any other region on Earth. Putting this rapid warming into
perspective is challenging because instrumental records are often short or incomplete in …

Climate in the Arctic region and northwestern Europe is strongly affected by the North
Atlantic Oscillation,(NAO), the dominant mode of atmospheric variability at mid-latitudes in …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …