# Touchan - Fenton Lake Recollection - PSME - ITRDB NM587 #----------------------------------------------------------------------- # 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/9700 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/northamerica/usa/nm587a-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/northamerica/usa/nm587a.crn # Description: Chronology - Tucson Decadal File # # Archive: Tree Ring # # Dataset_DOI: # # Parameter_Keywords: ring width #------------------- # Contribution_Date # Date: 2010-10-30 #------------------- # File_Last_Modified_Date # Date: 2018-12-20 #------------------- # Title # Study_Name: Touchan - Fenton Lake Recollection - PSME - ITRDB NM587 #------------------- # Investigators: Touchan, R.; Woodhouse, C.A.; Meko, D.M.; Allen, C. #------------------- # Description_Notes_and_Keywords # Description: NOAA Template Chronology file added 2018-12-20. #------------------- # Publication # Authors: # Journal_Name: International Journal of Climatology # Published_Title: Millennial precipitation reconstruction for the Jemez Mountains, New Mexico, reveals changing drought signal # Published_Date_or_Year: 2010 # Volume: # Pages: # Report_Number: # DOI: 10.1002/joc.2117 # Full_Citation: Touchan, R., C.A. Woodhouse, D.M. Meko, and C. Allen. 2010. Millennial precipitation reconstruction for the Jemez Mountains, # New Mexico, reveals changing drought signal. # Int. J. Climatol. Published on line 23 March 2010 # Abstract: Drought is a recurring phenomenon in the American Southwest. Since the frequency and severity of hydrologic droughts and other hydroclimatic events are of critical importance to the ecology and rapidly growing human population of this region, knowledge of long-term natural hydroclimatic variability is valuable for resource managers and policy-makers. An October-June precipitation reconstruction for the period AD 824-2007 was developed from multi-century tree-ring records of Pseudotsuga menziesii (Douglas-fir), Pinus strobiformis (Southwestern white pine) and Pinus ponderosa (Ponderosa pine) for the Jemez Mountains in Northern New Mexico. Calibration and verification statistics for the period 1896-2007 show a high level of skill, and account for a significant portion of the observed variance (>50%) irrespective of which period is used to develop or verify the regression model. Split-sample validation supports our use of a reconstruction model based on the full period of reliable observational data (1896-2007). A recent segment of the reconstruction (2000-2006) emerges as the driest 7-year period sensed by the trees in the entire record. That this period was only moderately dry in precipitation anomaly likely indicates accentuated stress from other factors, such as warmer temperatures. Correlation field maps of actual and reconstructed October-June total precipitation, sea surface temperatures and 500-mb geopotential heights show characteristics that are similar to those indicative of El Ni?o-Southern Oscillation patterns, particularly with regard to ocean and atmospheric conditions in the equatorial and north Pacific. Our 1184-year reconstruction of hydroclimatic variability provides long-term perspective on current and 20th century wet and dry events in Northern New Mexico, is useful to guide expectations of future variability, aids sustainable water management, provides scenarios for drought planning and as inputs for hydrologic models under a broader range of conditions than those provided by historical climate records. #------------------- # Site_Information # Site_Name: Fenton Lake # Location: New Mexico # Northernmost_Latitude: 35.88 # Southernmost_Latitude: 35.88 # Easternmost_Longitude: -106.67 # Westernmost_Longitude: -106.67 # Elevation: 2560 #------------------- # Data_Collection # Collection_Name: NM587 # Earliest_Year: 1304 # Most_Recent_Year: 2007 # Time_Unit: AD # Notes: #------------------- # Species # Species_Name: Pseudotsuga menziesii (Mirb.) Franco # Common_Name: Douglas-fir # Tree_Species_Code: PSME #------------------- # Chronology_Information # Chronology: #--------------------- # Variables # variables format: shortname var components: what,material,error,units,season,archive,detail,method, C or N for Char or Numeric data,additional information ## age_CE age,,,year Common Era,,tree ring,,,N, ## trsgi tree ring standardized growth index,,,,,tree ring,composited,ARSTAN,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1303 1328 1 1304 880 1 1305 840 1 1306 866 1 1307 397 1 1308 718 1 1309 744 1 1310 413 1 1311 896 1 1312 509 1 1313 797 1 1314 1247 1 1315 807 1 1316 496 1 1317 843 1 1318 680 1 1319 670 1 1320 873 1 1321 1043 1 1322 1241 1 1323 782 1 1324 783 1 1325 2052 1 1326 1092 1 1327 1356 1 1328 872 1 1329 1431 1 1330 1344 1 1331 1013 1 1332 1002 1 1333 1925 1 1334 1190 1 1335 639 1 1336 1308 1 1337 1534 1 1338 645 1 1339 1267 1 1340 1130 1 1341 1075 1 1342 492 1 1343 1354 1 1344 932 1 1345 619 1 1346 1190 1 1347 416 1 1348 548 1 1349 979 1 1350 923 1 1351 1264 1 1352 850 1 1353 1290 1 1354 931 1 1355 751 1 1356 1317 1 1357 1180 1 1358 1336 1 1359 930 1 1360 593 1 1361 939 1 1362 610 1 1363 554 1 1364 525 1 1365 1031 1 1366 1018 1 1367 549 1 1368 1291 1 1369 652 1 1370 941 1 1371 1055 1 1372 1554 1 1373 1251 1 1374 1182 1 1375 978 1 1376 918 1 1377 966 1 1378 1239 1 1379 1554 1 1380 1440 1 1381 878 1 1382 780 1 1383 1370 1 1384 909 1 1385 998 1 1386 1551 1 1387 1287 1 1388 1575 1 1389 1391 1 1390 1397 1 1391 1178 1 1392 1575 1 1393 1170 1 1394 1373 1 1395 1136 1 1396 1575 1 1397 1049 1 1398 875 1 1399 832 1 1400 795 1 1401 1071 1 1402 1085 1 1403 1524 1 1404 1065 1 1405 655 1 1406 1162 1 1407 881 1 1408 1195 1 1409 1121 1 1410 900 1 1411 658 1 1412 783 2 1413 896 2 1414 988 2 1415 895 2 1416 665 2 1417 836 2 1418 560 2 1419 596 2 1420 644 2 1421 1005 2 1422 1069 2 1423 701 2 1424 763 2 1425 1049 2 1426 1054 2 1427 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