The spatial and temporal complexity of the Holocene thermal maximum
By Hans Renssen, Heikki Seppä, O. Heiri, D. Roche, Hugues Goosse, T. Fichefet. 2009
561 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Environmental Chemistry
View Paper: https://www.semanticscholar.org/paper/748a1b3d97f675648dd601963c060b799e940bea
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In Atmospheric Science
In Environmental Chemistry
Citations in the corpus
- Global characterization of the Holocene Thermal Maximum (2012, methodology): “At mid-to-high latitudes of the Northern Hemisphere, the spatio-temporal complexity of the HTM can be explained by the cooling effect of the LIS, delaying the HTM by 1e2 thousand years compared to the orbitally-forced insolation maximum, particularly in NE North America, the North Atlantic, Western ”
- The past ecology of Abies alba provides new perspectives on future responses of silver fir forests to global warming (2013, background): “Dynamic climatic models are in good agreement with the paleoclimatic evidence and suggest a mid-Holocene thermal maximum at ca. 7000 November 2013 433PALEOECOLOGY, ABIES ALBA, AND THE FUTURE R E V IE W S cal yr BP over Europe (Renssen et al. 2009).”