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Charman and Hendon 2000 Water Table Depths in N.England Peatlands
Originator:
Charman, D.J.; Hendon, D.Citation Information:
Charman, D.J. and Hendon, D. 2000. Long-term changes in soil water tables over the past 4500 years: Relationships with climate and North Atlantic atmospheric circulation and sea surface temperature. Climatic Change, 47(1-2), 45-59. doi: 10.1023/A:1005673624994
NOAA Study Page:
https://www.ncei.noaa.gov/access/paleo-search/study/6333Lat:0, Lon:0
Use Constraints:
Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.Distributor:
National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of CommerceResource Description (data set id):
noaa-recon-6333Data Coverage:
Southernmost Latitude: 55.083333
Northernmost Latitude: 55.1
Westernmost Longitude: -2.5
Easternmost Longitude: -2.466667
Minimum Elevation: 280 m
Maximum Elevation: 325 m
Earliest Year: 4950 cal yr BP (-3000 CE)
Most Recent Year: -45 cal yr BP (1995 CE)
Northernmost Latitude: 55.1
Westernmost Longitude: -2.5
Easternmost Longitude: -2.466667
Minimum Elevation: 280 m
Maximum Elevation: 325 m
Earliest Year: 4950 cal yr BP (-3000 CE)
Most Recent Year: -45 cal yr BP (1995 CE)
Science Keywords:
Other Hydroclimate Reconstruction
Parameters:
earth science>paleoclimate>reconstructions
Variables:
data type | what | material | unit | seasonality | method | info |
---|---|---|---|---|---|---|
CLIMATE RECONSTRUCTIONSPALEOLIMNOLOGY | age | year Common Era | ||||
CLIMATE RECONSTRUCTIONSPALEOLIMNOLOGY | water table depth | testate amoebae assemblage | centimeter | annual | regression analysis | calibration data set: Woodland et al. 1998; weighted averaging regression |
Summary/Abstract:
A record of mean annual water table changes in England over the past 4500 years is derived from a transfer function applied to protozoan assemblages in peat profiles. A 100-year running mean value based on three profiles shows short-term changes which are closely related to instrumental records of mean annual temperature changes (past 300 yr) and documentary records of summer wetness and winter severity (past900 yr). Long-term (>1000 yr) changes in this composite record are positively correlated with the GISP2 ice accumulation record, suggesting moisture budgets were in phase across the North Atlantic region over at least the last 2000 years and probably changed due to north-south movements of major pressure centres. This hypothesis is further supported by comparisons with indicators of sea surface temperature and ocean circulation. Existing regional climate predictions may underestimate the impact of future warming on soil moisture status, with significant implications for agriculture and water supply in northwestern Europe.
More Information:
Contact Information:
DOC/NOAA/NESDIS/NCEI
National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
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USA
email: paleo@noaa.gov
phone: 828-271-4800 fax: 303-497-6513