RealClimate

Climate science from climate scientists...

You are here: Home / Archives for mike

mike

OK, But we do know it was warmer than present 6000 years ago, don’t we? Sommes nous sûrs qu’il faisait plus chaud il y a 6000 ans ?

by

This is yet another oft-repeated but problematic assertion based in this case on the mis-characterization of the so-called Mid-Holocene Climatic Optimum” or “Mid-Holocene Warm Period”. Paleoclimate experts now know that the mid-Holocene warmth centered roughly 8000 to 6000 years ago was probably restricted to high latitudes and certain seasons (summer in the Northern Hemisphere and winter in the southern hemisphere). Because much of the early paleoclimate evidence that was available (for example, fossil pollen assemblages) came from the Northern Hemisphere extratropics, and is largely reflective of summer conditions, decades ago some scientists believed that this was a time of globally warmer conditions. More abundant evidence now demonstrates, for example, that the tropical regions were cooler over much of the year.

par Michael Mann (traduit par Thibault de Garidel)

Cette assertion est très souvent répétée mais reste problématique en raison de la mauvaise caractérisation de cette période appelée ““Optimum climatique de l’Holocène moyen” ou “période chaude de l’Holocène moyen”. Les experts des paléoclimats, savent maintenant que cette phase chaude à l’Holocène (il y a approximativement 8000 à 6000 ans) était probablement limitée aux hautes latitudes et à certaines saisons (été dans l’hémisphère nord et hiver dans l’hémisphère sud). Comme la majorité des indicateurs du climat passé disponibles (comme par exemple, assemblages de pollens fossiles) provenaient des latitudes moyennes à hautes de l’hémisphère Nord, et étaient diagnostiques des condition climatiques d’été, certains scientifiques ont cru que cette période de temps était plus chaude globalement. Cependant, désormais, de nombreuses études montrent que les régions tropicales étaient plus fraîches pendant la plus grande partie de l’année.
(suite…)

[Read more…] about OK, But we do know it was warmer than present 6000 years ago, don’t we? Sommes nous sûrs qu’il faisait plus chaud il y a 6000 ans ?

Michael E. Mann

by

Dr. Michael E. Mann is Presidential Distinguished Professor in the Department of Earth and Environmental Science at the University of Pennsylvania, with a secondary appointment in the Annenberg School for Communication. He is director of the Penn Center for Science, Sustainability, and the Media (PCSSM).

Dr. Mann received his undergraduate degrees in Physics and Applied Math from the University of California at Berkeley, an M.S. degree in Physics from Yale University, and a Ph.D. in Geology & Geophysics from Yale University. His research involves the use of theoretical models and observational data to better understand Earth’s climate system.

Dr. Mann was a Lead Author on the Observed Climate Variability and Change chapter of the Intergovernmental Panel on Climate Change (IPCC) Third Scientific Assessment Report in 2001 and was organizing committee chair for the National Academy of Sciences Frontiers of Science in 2003. He has received a number of honors and awards including NOAA’s outstanding publication award in 2002 and selection by Scientific American as one of the fifty leading visionaries in science and technology in 2002. He contributed, with other IPCC authors, to the award of the 2007 Nobel Peace Prize. He was awarded the Hans Oeschger Medal of the European Geosciences Union in 2012 and was awarded the National Conservation Achievement Award for science by the National Wildlife Federation in 2013. He made Bloomberg News’ list of fifty most influential people in 2013. In 2014, he was named Highly Cited Researcher by the Institute for Scientific Information (ISI) and received the Friend of the Planet Award from the National Center for Science Education. He received the Stephen H. Schneider Award for Outstanding Climate Science Communication from Climate One in 2017, the Award for Public Engagement with Science from the American Association for the Advancement of Science in 2018 and the Climate Communication Prize from the American Geophysical Union in 2018. In 2019 he received the Tyler Prize for Environmental Achievement and in 2020 he received the World Sustainability Award of the MDPI Sustainability Foundation. He was elected to the U.S. National Academy of Sciences in 2020. He is a Fellow of the American Geophysical Union, the American Meteorological Society, the Geological Society of America, the American Association for the Advancement of Science, and the Committee for Skeptical Inquiry. He is also a co-founder of the award-winning science website RealClimate.org.

Dr. Mann is author of more than 200 peer-reviewed and edited publications, numerous op-eds and commentaries, and four books including Dire Predictions: Understanding Climate Change, The Hockey Stick and the Climate Wars: Dispatches from the Front Lines, The Madhouse Effect, The Tantrum that Saved the World and The New Climate War; He is co-founder of RealClimate.

More information about his research and publication record can be found here.

All posts by mike.

Temperature Variations in Past Centuries and the so-called "Hockey Stick" Variations de température sur les derniers siècles et la "crosse de hockey"

by

Instrumental data describing large-scale surface temperature changes are only available for roughly the past 150 years. Estimates of surface temperature changes further back in time must therefore make use of the few long available instrumental records or historical documents and natural archives or ‘climate proxy’ indicators, such as tree rings, corals, ice cores and lake sediments, and historical documents to reconstruct patterns of past surface temperature change. Due to the paucity of data in the Southern Hemisphere, recent studies have emphasized the reconstruction of Northern Hemisphere (NH) mean, rather than global mean temperatures over roughly the past 1000 years.


par Mike Mann (traduit par Gilles Delaygue)
Les données intrumentales décrivant les changements à grande échelle de la température de surface ne sont disponibles que pour les derniers 150 ans environ. Pour estimer des changements de température de surface antérieurs, il faut ainsi utiliser les quelques longs enregistrements disponibles, ou des documents historiques, ainsi que des archives naturelles ou proxies climatiques, comme les cernes d’arbres, coraux, carottes de glace et sédiments lacustres, pour reconstruire les changements de température dans le passé. En raison de la rareté des données dans l’hémisphère sud, les études récentes ont été focalisées sur les reconstructions de moyennes pour l’hémisphère nord, plutôt que globales, sur les derniers 1000 ans environ.

[Read more…] about Temperature Variations in Past Centuries and the so-called "Hockey Stick" Variations de température sur les derniers siècles et la "crosse de hockey"

False Claims by McIntyre and McKitrick regarding the Mann et al. (1998) reconstruction

by

A number of spurious criticisms regarding the Mann et al (1998) proxy-based temperature reconstruction have been made by two individuals McIntyre and McKitrick ( McIntyre works in the mining industry, while McKitrick is an economist). These criticisms are contained in two manuscripts (McIntyre and McKitrick 2003 and 2004–the latter manuscript was rejected by Nature; both are collectively henceforth referred to as “MM”). MM claim that the main features of the Mann et al (1998–henceforth MBH98) reconstruction, including the “hockey stick” shape of the reconstruction, are artifacts of a) the centering convention used by MBH98 in their Principal Components Analysis (PCA) of the North American International Tree Ring Data Bank (‘ITRDB’) data, b) the use of 4 infilled missing annual values (AD 1400-1403) in one tree-ring series (the ‘St. Anne’ Northern Treeline series), and c) the infilling of missing values in some proxy data between 1972 and 1980. Each of these claims are demonstrated to be false below. [Read more…] about False Claims by McIntyre and McKitrick regarding the Mann et al. (1998) reconstruction

CO2 Fertilization

by

It has sometimes been argued that the earth’s biosphere (in large part, the terrestrial biosphere) may have the capacity to sequestor much of the increased carbon dioxide (CO2) in the atmosphere associated with human fossil fuel burning. This effect is known as “CO2 fertilization” because, in the envisioned scenario, higher ambient CO2 concentrations in the atmosphere literally “fertilize” plant growth. Because plants in turn, in the process of photosynthesis, convert CO2 into oxygen, it is thus sometimes argued that such “co2 fertilization” could potentially provide a strong negative feedback on changing CO2 concentrations.

[Read more…] about CO2 Fertilization

Rutherford et al 2005 highlights

by

The claims of McIntyre and McKitrick regarding the Mann et al (1998) temperature reconstruction have recently been discredited by the following peer-reviewed article to appear in the American Meteorological Society journal, “Journal of Climate“:

Rutherford, S., Mann, M.E., Osborn, T.J., Bradley, R.S., Briffa, K.R., Hughes, M.K., Jones, P.D., Proxy-based Northern Hemisphere Surface Temperature Reconstructions: Sensitivity to Methodology, Predictor Network, Target Season and Target Domain, Journal of Climate, in press (2005).

Key excerpts from the article are provided below: [Read more…] about Rutherford et al 2005 highlights