# Melvin - Radley - QUSP - ITRDB BRIT061 #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite original publication, online resource and date accessed when using these data, # If there is no publication information, please cite investigator, title, online resource and date accessed. # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/13750 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/brit061-noaa.rwl # Description: Raw Measurements - NOAA Template File # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/brit061.rwl # Description: Raw Measurements - Tucson Decadal File # # Archive: Treering # # Dataset_DOI: # # Parameter_Keywords: ring width #------------------- # Contribution_Date # Date: 2012-05-01 #------------------- # File_Last_Modified_Date # Date: 2019-02-05 #------------------- # Title # Study_Name: Melvin - Radley - QUSP - ITRDB BRIT061 #------------------- # Investigators: Melvin, T.M.; Briffa, K.R. #------------------- # Description_Notes_and_Keywords # Description: NOAA Template Raw Measurements file added 2019-02-05. #------------------- # Publication # Authors: # Journal_Name: Climate Dynamics # Published_Title: A millennial long March-July precipitation reconstruction for southern-central England # Published_Date_or_Year: 2012 # Volume: # Pages: # Report_Number: # DOI: 10.1007/s00382-012-1318-z # Full_Citation: Wilson, R., D. Miles, N.J. Loader, T. Melvin, L. Cunningham, # R. Cooper, and K. Briffa. 2012. # A millennial long March-July precipitation reconstruction # for southern-central England. # Climate Dynamics, Vol. 40, Issue 3-4, pp. 997-1017, February 2013. # doi:10.1007/s00382-012-1318-z # Abstract: We present a millennial long dendroclimatic reconstruction # of spring/summer precipitation for southern-central England. # Previous research identified a significant moisture stress # signal in ring-width data measured from oak trees growing # in southern England. In this study, we build upon this earlier # work, specifically targeting south-central England, to derive # a well replicated oak ring-width composite chronology using # both living and historical material. The data-set includes # 352 living trees (AD 1629-2009) and 1540 individual historical # series (AD 663-1925). The period expressed by at least 50 trees # in any year is AD 980-2009. Calibration experiments identify # the optimal seasonal predictand target as March-July precipitation # (1901-2007: r2 = 0.33). However, comparison with the long Kew # Gardens precipitation record indicates a weakening in tree-growth/ # climate response from ~1800 to 1920 which we speculate may be # related to smoke and sulphur dioxide (SO2) emissions at that # time which may have also contributed to a decrease in tree # productivity. The time-series derived using the regional curve # standardisation method to capture lower frequency information # shows a mediaeval period with alternating multi-decade-long dry # and wet periods, with AD 1153-1172 being the wettest reconstructed # 20-year period in the whole record. Drier conditions are prevalent # from ~1300 to the early sixteenth century followed by a period of # increasing precipitation levels. The most recent four centuries # of the record appear similar to the mediaeval period with multiple # decade-long dry and wet periods. The late twentieth century is # the second reconstructed wettest period. These centennial # hydroclimatic trends are in broad agreement with independent # regional scale hydroclimatic reconstructions from tree-ring # (East Anglia), historical, speleothem and peat water level # proxy archives in the United Kingdom and appear coupled # with reconstructed sea surface temperature changes in the # North Atlantic which in turn influence the Atlantic meridional # overturning circulation and westerly airflow across the UK. #------------------- # Site Information # Site_Name: Radley # Location: United Kingdom # Northernmost_Latitude: 51.7 # Southernmost_Latitude: 51.7 # Easternmost_Longitude: -1.2167 # Westernmost_Longitude: -1.2167 # Elevation: 70 #------------------- # Data Collection # Collection_Name: BRIT061 # Earliest_Year: 1812 # Most_Recent_Year: 1979 # Time_Unit: AD # Notes: #------------------- # Species # Species_Name: Quercus spp. L. # Common_Name: oak # Tree_Species_Code: QUSP #------------------- # Chronology_Information # Chronology: #--------------------- # Variables # Data variables follow that are preceded by '##' in columns one and two. # Variables list, one per line; shortname-tab- components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data,additional information) ## age_CE age,,,year Common Era,,tree ring,,,N, ## KC01AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC01AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC02AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC02AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC03AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC03AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC04AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC04AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC07AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC07AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC08AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC08AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC09AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC09AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC10AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC10AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC11AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC11AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC13AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC13AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC14AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC14AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC15AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC15AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC17AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC17AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC18AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC18AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC19AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC19AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC20AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC20AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC21AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC21AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 ## KC22AA_raw total ring width ,,,millimeter,,tree ring,,,N,Tree ID: KC22AA; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999 #--------------------- # Data: # Missing_Values: NA age_CE KC01AA_raw KC02AA_raw KC03AA_raw KC04AA_raw KC07AA_raw KC08AA_raw KC09AA_raw KC10AA_raw KC11AA_raw KC13AA_raw KC14AA_raw KC15AA_raw KC17AA_raw KC18AA_raw KC19AA_raw KC20AA_raw KC21AA_raw KC22AA_raw 1812 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 412 NaN 1813 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 305 NaN 1814 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 222 NaN 1815 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 298 NaN 1816 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 253 NaN 1817 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 161 NaN 1818 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 194 NaN 1819 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 457 NaN 1820 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 210 NaN 1821 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 229 NaN 1822 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 303 NaN 1823 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 405 NaN 1824 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 322 NaN 1825 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 206 NaN NaN NaN 234 NaN 1826 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 199 NaN NaN NaN 237 NaN 1827 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 305 NaN NaN NaN 305 NaN 1828 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 312 NaN NaN NaN 360 NaN 1829 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 246 NaN NaN NaN 267 NaN 1830 208 NaN NaN NaN 258 NaN NaN NaN NaN NaN NaN NaN 324 NaN NaN NaN 334 NaN 1831 163 NaN NaN NaN 137 NaN NaN NaN NaN NaN NaN NaN 220 NaN NaN NaN 225 NaN 1832 182 NaN NaN NaN 165 199 NaN NaN NaN NaN NaN NaN 229 NaN NaN NaN 267 NaN 1833 199 NaN NaN NaN 132 139 NaN NaN NaN NaN NaN NaN 201 NaN NaN NaN 234 NaN 1834 258 NaN NaN NaN 220 180 NaN NaN NaN NaN NaN NaN 284 NaN NaN 457 412 NaN 1835 201 NaN NaN NaN 253 111 NaN NaN NaN NaN NaN NaN 286 NaN NaN 291 386 NaN 1836 161 NaN NaN NaN 227 85 NaN NaN NaN NaN NaN NaN 239 NaN NaN 319 474 161 1837 194 NaN NaN NaN 265 78 NaN NaN NaN NaN NaN 52 248 NaN NaN 329 374 120 1838 144 NaN NaN NaN 184 68 NaN NaN NaN NaN NaN 59 165 NaN NaN 208 182 66 1839 151 NaN NaN NaN 82 90 NaN NaN NaN NaN NaN 146 158 NaN NaN 554 277 73 1840 127 NaN NaN NaN 87 101 NaN NaN NaN NaN 113 66 142 NaN NaN 130 151 52 1841 97 NaN NaN NaN 63 196 NaN NaN NaN NaN 149 73 97 NaN NaN 104 80 135 1842 94 NaN NaN NaN 75 149 NaN NaN NaN NaN 168 94 73 NaN NaN 194 97 120 1843 132 NaN NaN NaN 75 227 NaN NaN NaN NaN 194 227 191 203 NaN 291 85 75 1844 90 NaN NaN NaN 63 130 NaN NaN NaN NaN 191 90 118 85 NaN 180 78 56 1845 123 NaN NaN NaN 101 206 NaN NaN NaN NaN 286 201 244 165 NaN 293 151 170 1846 104 NaN NaN NaN 61 149 NaN NaN NaN NaN 180 123 149 168 NaN 218 82 120 1847 220 NaN NaN NaN 113 234 NaN NaN NaN NaN 329 206 210 201 NaN 289 125 165 1848 282 NaN 308 NaN 165 317 NaN NaN NaN NaN 381 277 267 244 NaN 393 180 206 1849 239 NaN 267 NaN 232 303 NaN 142 NaN NaN 438 248 327 246 NaN 343 234 151 1850 222 NaN 218 NaN 229 414 NaN 125 NaN NaN 391 260 308 308 NaN 374 156 135 1851 199 NaN 218 NaN 225 353 NaN 90 189 NaN 317 267 220 308 NaN 305 187 184 1852 175 NaN 184 NaN 246 381 NaN 135 199 NaN 282 258 225 300 NaN 222 116 127 1853 168 NaN 229 NaN 248 410 NaN 170 215 NaN 315 324 263 343 NaN 364 142 165 1854 142 NaN 142 NaN 189 310 265 137 239 NaN 284 234 165 289 NaN 206 139 149 1855 175 NaN 161 NaN 312 369 341 248 410 NaN 419 312 210 417 NaN 374 210 222 1856 291 NaN 293 NaN 277 346 279 272 410 NaN 350 343 303 431 NaN 331 222 251 1857 305 NaN 343 NaN 341 376 329 279 381 NaN 410 303 258 476 NaN 350 258 248 1858 227 NaN 248 NaN 218 282 277 248 400 NaN 372 253 260 310 NaN 412 346 300 1859 258 NaN 191 NaN 315 319 315 274 485 NaN 400 355 284 331 NaN 327 293 272 1860 220 NaN 208 NaN 282 317 267 234 327 NaN 279 336 308 336 NaN 246 222 300 1861 175 NaN 180 NaN 263 357 173 104 173 NaN 277 296 229 244 NaN 315 173 329 1862 170 367 149 317 130 241 210 163 282 NaN 218 284 251 315 NaN 227 196 324 1863 253 469 296 447 154 315 213 191 305 NaN 246 293 232 286 NaN 305 182 277 1864 341 599 334 528 199 272 227 248 353 500 317 291 210 300 NaN 279 277 274 1865 343 732 393 514 405 310 274 310 623 443 402 405 421 526 459 476 282 300 1866 317 568 343 511 360 502 312 350 561 720 419 336 462 462 426 483 346 338 1867 220 639 289 488 414 355 350 405 500 637 417 317 462 376 405 402 362 412 1868 255 393 270 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