# 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/nm587r-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/northamerica/usa/nm587r.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,residual,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1305 832 1 1306 913 1 1307 442 1 1308 862 1 1309 866 1 1310 497 1 1311 1048 1 1312 592 1 1313 913 1 1314 1341 1 1315 775 1 1316 512 1 1317 972 1 1318 765 1 1319 755 1 1320 976 1 1321 1104 1 1322 1245 1 1323 726 1 1324 805 1 1325 2121 1 1326 888 1 1327 1228 1 1328 786 1 1329 1422 1 1330 1264 1 1331 895 1 1332 964 1 1333 1923 1 1334 992 1 1335 504 1 1336 1366 1 1337 1505 1 1338 499 1 1339 1288 1 1340 1109 1 1341 1019 1 1342 463 1 1343 1455 1 1344 908 1 1345 597 1 1346 1279 1 1347 414 1 1348 654 1 1349 1136 1 1350 974 1 1351 1282 1 1352 802 1 1353 1296 1 1354 884 1 1355 737 1 1356 1378 1 1357 1137 1 1358 1265 1 1359 839 1 1360 573 1 1361 1034 1 1362 665 1 1363 644 1 1364 660 1 1365 1179 1 1366 1060 1 1367 542 1 1368 1386 1 1369 635 1 1370 986 1 1371 1103 1 1372 1549 1 1373 1126 1 1374 1071 1 1375 913 1 1376 904 1 1377 986 1 1378 1255 1 1379 1506 1 1380 1297 1 1381 726 1 1382 761 1 1383 1430 1 1384 852 1 1385 980 1 1386 1561 1 1387 1169 1 1388 1457 1 1389 1238 1 1390 1255 1 1391 1053 1 1392 1496 1 1393 1028 1 1394 1277 1 1395 1039 1 1396 1508 1 1397 912 1 1398 805 1 1399 853 1 1400 844 1 1401 1132 1 1402 1091 1 1403 1499 1 1404 943 1 1405 588 1 1406 1229 1 1407 881 1 1408 1204 1 1409 1091 1 1410 854 1 1411 667 1 1412 867 2 1413 977 2 1414 1032 2 1415 909 2 1416 688 2 1417 919 2 1418 629 2 1419 707 2 1420 776 2 1421 1123 2 1422 1105 2 1423 686 2 1424 820 2 1425 1131 2 1426 1068 2 1427 1002 2 1428 1343 2 1429 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