Reconstructing Climates of the QuaternaryBy
- Raymond Bradley
Undergraduates, researchers, lecturers, professionals and classes in archeology, palynology, geology, geosciences, geological research methods, paleoecology, paleooceanography, paleoclimatology, climatology, climate modeling, glaciology, geomorphology, geography, earth sciences, environmental sciences, oceanography, astronomy, meteorology and Quaternary sciences; archeologists, scientists, and government and agency officials who deal with issues of global environmental change.
Hardbound, 613 Pages
Published: February 1999
Imprint: Academic Press
"An indispensable work of reference for scientists and students alike."
Praise for the first edition:, --Quarternary Science Reviews
"There can be little doubt that overall this book is a great success in the way the information is assimilated, explained and placed in a global context."
--Journal of Quarternary Science
"A book which ought to be read as a primer by anyone with a critical interest in the field."
--Earth Surface Processes and :Landforms
"Unrivaled in the sophistication with which it examines a wide range of methods."
--K.W. Butzer, Journal of Archeological Science
"A resounding success... indispensable reading for anyone involved in paleoclimatic reconstruction or paleoclimatic modeling."
--L.D.D. Harvey, University of Toronto
Published Review As reviewed in CHOICE, October 1999 "Bradley's new edition (1st ed., Quaternary Paleoclimatology, CH, Jul'85) is a thorough update; there is new material on ice cores, better dating, marine sediments, ocean circulations, corals, and paleoclimate models. About 2,000 references are listed, with more than half newer than 1985. This is an excellent compilation of figures and tables covering the entire subject. Many subtopics are of interest to casual readers: El NiÃ±os (Ninos) since 1525; extent and seasonal changes in snow-ice cover; paleomagnetism--dates of major reversals in polarity; dust veil index since 1500, corresponding to volcanic activity; information from tree rings; ocean temperatures and salinity affecting the conveyor belt circulation; lake and sea level fluctuations; pollen analysis; and variability in flowering dates of plants and grape harvests. Surprisingly, some climate changes have been rapid and vegetation changes lag behind climate changes by 100 to 150 years. One of the problems in coupled ocean-atmosphere models is that response times for various components vary by six to seven orders of magnitude. This new edition is needed by college libraries. General readers; upper-division undergraduates through faculty." â A. E. Staver, Northern Illinois Universit