# 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/nm587-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/northamerica/usa/nm587.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,standard,N, ## numsamp number of samples,,,count,,tree ring,,,N, # #-------------------- # Data: # Missing_Values: -999 age_CE trsgi numsamp 1304 1328 1 1305 880 1 1306 882 1 1307 411 1 1308 747 1 1309 811 1 1310 453 1 1311 942 1 1312 571 1 1313 827 1 1314 1300 1 1315 818 1 1316 470 1 1317 868 1 1318 732 1 1319 697 1 1320 913 1 1321 1079 1 1322 1249 1 1323 759 1 1324 753 1 1325 2068 1 1326 1067 1 1327 1230 1 1328 817 1 1329 1379 1 1330 1321 1 1331 941 1 1332 944 1 1333 1903 1 1334 1141 1 1335 519 1 1336 1271 1 1337 1543 1 1338 584 1 1339 1205 1 1340 1135 1 1341 1033 1 1342 459 1 1343 1349 1 1344 960 1 1345 580 1 1346 1195 1 1347 439 1 1348 544 1 1349 1045 1 1350 972 1 1351 1267 1 1352 839 1 1353 1257 1 1354 919 1 1355 712 1 1356 1317 1 1357 1183 1 1358 1287 1 1359 880 1 1360 542 1 1361 943 1 1362 645 1 1363 571 1 1364 574 1 1365 1094 1 1366 1067 1 1367 544 1 1368 1295 1 1369 677 1 1370 918 1 1371 1079 1 1372 1552 1 1373 1214 1 1374 1099 1 1375 921 1 1376 879 1 1377 955 1 1378 1237 1 1379 1537 1 1380 1382 1 1381 784 1 1382 713 1 1383 1369 1 1384 907 1 1385 953 1 1386 1542 1 1387 1255 1 1388 1492 1 1389 1315 1 1390 1300 1 1391 1096 1 1392 1503 1 1393 1107 1 1394 1286 1 1395 1079 1 1396 1512 1 1397 992 1 1398 794 1 1399 807 1 1400 800 1 1401 1087 1 1402 1096 1 1403 1505 1 1404 1022 1 1405 581 1 1406 1145 1 1407 897 1 1408 1175 1 1409 1112 1 1410 646 2 1411 478 2 1412 613 2 1413 740 2 1414 820 2 1415 711 2 1416 479 2 1417 653 2 1418 397 2 1419 421 2 1420 474 2 1421 845 2 1422 945 2 1423 613 2 1424 732 2 1425 1083 2 1426 1148 2 1427 1165 2 1428 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