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The World Data Center for Paleoclimatology features newly archived paleoclimatic data
and climate reconstructions relevant to important issues in paleoclimatology,
plus new services we offer to the scientific community. For a complete listing of
recent data contributions, please click the "most recent ten contributions" link on our
Contribution Series Search page
Please check our archived pages for What's New sections for the years: 2007, 2006, 2005, 2004, 2003, 2002, 2001, 2000, 1999, 1998, 1997, 1996, and 1995. What's New for 2008: |
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Palaeoclimate
Jansen et al. IPCC Fourth Assessment, Working Group 1 In Solomon et al. Climate Change 2007: The Physical Science Basis. Cambridge University Press, Cambridge, UK and New York, NY, USA. This chapter assesses palaeoclimatic data and knowledge of how the climate system changes over interannual to millennial time scales, and how well these variations can be simulated with climate models. Additional palaeoclimatic perspectives are included in other chapters. Palaeoclimate science has made significant advances since the 1970s, when a primary focus was on the origin of the ice ages, the possibility of an imminent future ice age, and the first explorations of the so-called Little Ice Age and Medieval Warm Period. Even in the first IPCC assessment (IPCC, 1990), many climatic variations prior to the instrumental record were not that well known or understood. Fifteen years later, understanding is much improved, more quantitative and better integrated with respect to observations and modelling. |
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A European pattern climatology 1766-2000
Casty et al. Climate Dynamics Volume 29, Numbers 7-8, December, 2007. doi:10.1007/s00382-007-0257-6 Using monthly independently reconstructed gridded European fields for the 500 hPa geopotential height, temperature, and precipitation covering the last 235 years we investigate the temporal and spatial evolution of these key climate variables and assess the leading combined patterns of climate variability. Seasonal European temperatures show a positive trend mainly over the last 40 years with absolute highest values since 1766. Precipitation indicates no clear trend. Spatial correlation technique reveals that winter, spring, and autumn covariability between European temperature and precipitation is mainly influenced by advective processes, whereas during summer convection plays the dominant role. The dominant patterns of climate variability for winter, spring, and autumn resemble the North Atlantic Oscillation and show a distinct positive trend during the past 40 years for winter and spring. A positive trend is also detected for summer pattern 2, which reflects an increased influence of the Azores High towards central Europe and the Mediterranean coinciding with warm and dry conditions. |
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Fire Climatology
Swetnam and Anderson eds. International Journal of Wildland Fire Special Issue Vol. 17. No. 1. February 2008 This issue of the International Journal of Wildland Fire highlights significant work presented at a session on fire climatology at the 3rd International Fire Ecology and Management Congress in San Diego, USA, in 2006. Manuscripts in this special issue have passed rigorous peer-review and offer more detail that presented at the Congress. A defining feature of this collection is the inclusion of both modern and palaeofire perspectives, working with a broad range of data over a range of temporal and spatial scales. Three themes therefore are: modern fire climatology from documentary records; palaeofire climatology from tree rings and fire scars; and palaeofire climatology from sedimentary charcoal and pollen. These themes provide contrasting or complementary insights about fire regime changes and responses to climate. |
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Grape harvest dates as a proxy for Swiss April to August temperature
reconstructions back to AD 1480
Meier et al. Geophysical Research Letters Vol. 34, L20705, doi:10.1029/2007GL031381 We present an annually resolved record of grape harvest dates for Switzerland. The strong negative relationship between grape harvest dates and April-August temperatures allowed a new reconstruction, with associated uncertainties, to be derived back to 1480. Calibration (1928-1979) was performed with monthly data from the Basel and Geneva stations and verified over 1980-2006. Twelve days of grape harvest difference correspond to around 1°C April-August temperature difference. Periods cooler (late grape harvest dates) than the 1961-1990 mean are reconstructed during the 17th century and at the beginning of the 19th century. Warmer conditions were experienced in the early 18th century and during the recent decades, in agreement with grape harvest temperature reconstructions from France and other independent temperature estimates. On decadal (annual) time-scales the earliest harvests were in the 1580s (2003) and the latest vintages in the 1740s (1816). Large tropical volcanic eruptions led to significantly later grape harvest dates (cooling) one to two years after the event. |
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http://www.ncdc.noaa.gov/paleo/whatsnew.html Downloaded Saturday, 10-May-2008 18:30:33 EDT Last Updated Friday, 04-Apr-2008 10:56:44 EDT by paleo@noaa.gov Please see the Paleoclimatology Contact Page or the NCDC Contact Page if you have questions or comments. |