By Harunur Rashid, Leonid Polyak, Ellen Mosley-Thompson
Published via the yankee Geophysical Union as a part of the Geophysical Monograph Series.Abrupt weather switch: Mechanisms, styles, and Impacts brings jointly a various team of paleoproxy documents resembling ice cores, marine sediments, terrestrial (lakes and speleothems) data, and matched ocean-atmosphere weather versions to record contemporary advances in knowing the mechanisms of abrupt weather adjustments. because the discovery of the Dansgaard-Oeschger occasions in Greenland ice cores and the following discovery in their modern occasions within the marine sediments of the North Atlantic, the hunt for those abrupt, millennial-scale occasions around the globe has intensified, and therefore, the variety of paleoclimatic files chronicling such occasions has elevated. the quantity highlights contain discussions of files of prior weather variability, meridional overturning...
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Extra resources for Abrupt Climate Change. Mechanisms, Patterns, and Impacts
INTRODUCTION 2. PREVIOUS HYPOTHESES 3. THE Δ14C RECORD AND THE TIMING OF ATMOSPHERIC CO2 CHANGE 4. ARE THERE OTHER SOURCES OF Δ14C-DEPLETED CARBON IN THE OCEAN? 5. AN OCEAN CO2 CAPACITOR? 6. STORAGE AND PRODUCTION OF CO2 DURING GLACIATIONS 7. A MECHANISM FOR CO2 RELEASE DURING DEGLACIATION 8. SUMMARY The Impact of the Final Lake Agassiz Flood Recorded in Northeast Newfoundland and Northern Scotian Shelves Based on Century-Scale Palynological Data 1. INTRODUCTION 2. REGIONAL SETTING 3. METHODS 4.
These records were selected based on the geographic location and temporal resolution adequate to assess millennial- or finerscale climate events. Regardless of the nature of climate archives, the climatic expression of the D-O cycles is evident from the southwest Pacific Ocean to northeastern Siberia. 2. Deglaciation Period One of the most studied periods of the last glacial cycle is the time between 10 and 25 ka, commonly known as the last deglaciation. 5 ka). The rationales behind focusing on the last deglaciation interval include the availability of paleoclimate records with high temporal resolution and a robust age control constrained by 14C–accelerator mass spectrometry and U-Th dating.
G. Thompson). (bottom) For the atmosphere, vectors depicting the winds in the lowest model layer and the sea level pressure. Ocean model surface temperatures are shown in blue to red colors; sea ice concentration is shown in white gray. This coupled model consists of the National Center for Atmospheric Research Community Climate Model for the atmospheric component, the Los Alamos National Laboratory Parallel Ocean Program for the ocean component, and the Naval Postgraduate School sea ice model (courtesy of G.
Abrupt Climate Change. Mechanisms, Patterns, and Impacts by Harunur Rashid, Leonid Polyak, Ellen Mosley-Thompson