# Woodhouse - Filmore Canyon - PIPO - ITRDB NM595 #----------------------------------------------------------------------- # 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/22321 # Description: NOAA Landing Page of study # Online_Resource: https://www1.ncdc.noaa.gov//pub/data/paleo/treering/chronologies/northamerica/usa/nm595-noaa.crn # Description: Chronology - NOAA Template File # # Original_Source_URL: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/chronologies/northamerica/usa/nm595.crn # Description: Chronology - Tucson Decadal File # # Archive: Tree Ring # # Dataset_DOI: # # Parameter_Keywords: ring width #------------------- # Contribution_Date # Date: 2016-07-07 #------------------- # File_Last_Modified_Date # Date: 2018-12-20 #------------------- # Title # Study_Name: Woodhouse - Filmore Canyon - PIPO - ITRDB NM595 #------------------- # Investigators: Woodhouse, C.A.; Losleben, M.V. #------------------- # Description_Notes_and_Keywords # Description: NOAA Template Chronology file added 2018-12-20. #------------------- # Publication # Authors: David W. Stahle, Edward R. Cook, Dorian J. Burnette, Jose Villanueva, Julian Cerano, Jordan N. Burns, Daniel Griffin, Benjamin I. Cook, Rodolfo Acuna, Max C.A. Torbenson, Paul Sjezner, Ian M. Howard # Journal_Name: Quaternary Science Reviews # Published_Title: The Mexican Drought Atlas: Tree-ring reconstructions of the soil moisture balance during the late pre-Hispanic, colonial, and modern eras # Published_Date_or_Year: 2016 # Volume: 149 # Pages: 34-60 # Report_Number: # DOI: 10.1016/j.quascirev.2016.06.018 # Full_Citation: # Abstract: Mexico has suffered a long history and prehistory of severe sustained drought. Drought over Mexico is modulated by ocean-atmospheric variability in the Atlantic and Pacific, raising the possibility for long-range seasonal climate forecasting, which could help mediate the economic and social impacts of future dry spells. The instrumental record of Mexican climate is very limited before 1920, but tree-ring chronologies developed from old-growth forests in Mexico can provide an excellent proxy representation of the spatial pattern and intensity of past moisture regimes useful for the analysis of climate dynamics and climate impacts. The Mexican Drought Atlas (MXDA) has been developed from an extensive network of 252 climate sensitive tree-ring chronologies in and near Mexico. The MXDA reconstructions extend from 1400 CE-2012 and were calibrated with the instrumental summer (JJA) self-calibrating Palmer Drought Severity Index (scPDSI) on a 0.5 latitude/longitude grid extending over land areas from 14 to 34N and 75-120W using Ensemble Point-by-Point Regression (EPPR) for the 1944-1984 period. The grid point reconstructions were validated for the period 1920-1943 against instrumental gridded scPDSI values based on the fewer weather station observations available during that interval. The MXDA provides a new spatial perspective on the historical impacts of moisture extremes over Mexico during the past 600-years, including the Aztec Drought of One Rabbit in 1454, the drought of El Ano de Hambre in 1785-1786, and the drought that preceded the Mexican Revolution of 1909-1910. # The El Nino/Southern Oscillation (ENSO) is the most important ocean-atmospheric forcing of moisture variability detected with the MXDA. In fact, the reconstructions suggest that the strongest central equatorial Pacific sea surface temperature (SST) teleconnection to the soil moisture balance over North America may reside in northern Mexico. This ENSO signal has stronger and more time-stable correlations than computed for either the Atlantic Multidecadal Oscillation or Pacific Decadal Oscillation. The extended Multivariate ENSO Index is most highly correlated with reconstructed scPDSI over northern Mexico, where warm events favor moist conditions during the winter, spring, and early summer. This ENSO teleconnection to northern Mexico has been strong over the past 150 years, but it has been comparatively weak and non-stationary in the MXDA over central and southern Mexico where eastern tropical Pacific and Caribbean/tropical Atlantic SSTs seem to be more important. The ENSO teleconnection to northern Mexico is weaker in the available instrumental PDSI, but analyses based on the millennium climate simulations with the Community Earth System Model suggest that the moisture balance during the winter, spring, and early summer over northern Mexico may indeed be particularly sensitive to ENSO forcing. Nationwide drought is predicted to become more common with anthropogenic climate change, but the MXDA reconstructions indicate that intense "All Mexico" droughts have been rare over the past 600 years and their frequency does not appear to have increased substantially in recent decades. #------------------- # Site_Information # Site_Name: Filmore Canyon # Location: New Mexico # Northernmost_Latitude: 32.334 # Southernmost_Latitude: 32.334 # Easternmost_Longitude: -106.562 # Westernmost_Longitude: -106.562 # Elevation: 2133 #------------------- # Data_Collection # Collection_Name: NM595 # Earliest_Year: 1306 # Most_Recent_Year: 2008 # Time_Unit: AD # Notes: #------------------- # Species # Species_Name: Pinus ponderosa Douglas ex C. Lawson # Common_Name: ponderosa pine # Tree_Species_Code: PIPO #------------------- # 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 1306 544 1 1307 1158 1 1308 958 1 1309 1050 1 1310 683 1 1311 1148 1 1312 1080 1 1313 630 1 1314 313 1 1315 928 1 1316 790 1 1317 472 1 1318 787 1 1319 1061 1 1320 1427 1 1321 1193 1 1322 1295 1 1323 1014 1 1324 805 1 1325 754 1 1326 867 1 1327 373 1 1328 378 1 1329 860 1 1330 802 1 1331 425 1 1332 534 1 1333 733 1 1334 788 1 1335 1151 1 1336 1134 1 1337 571 1 1338 856 1 1339 787 1 1340 694 1 1341 992 1 1342 1125 1 1343 1305 1 1344 1228 1 1345 715 1 1346 1313 1 1347 634 1 1348 754 1 1349 814 1 1350 700 1 1351 1030 1 1352 847 2 1353 1002 2 1354 1278 2 1355 862 2 1356 1310 2 1357 803 2 1358 944 2 1359 962 2 1360 650 2 1361 482 2 1362 568 2 1363 344 2 1364 596 2 1365 701 2 1366 721 2 1367 840 2 1368 1086 2 1369 966 2 1370 963 2 1371 775 2 1372 995 2 1373 688 2 1374 821 3 1375 599 4 1376 655 5 1377 1213 5 1378 928 5 1379 736 5 1380 985 5 1381 830 7 1382 577 7 1383 756 8 1384 834 8 1385 1802 8 1386 807 8 1387 592 8 1388 883 8 1389 1176 8 1390 1002 8 1391 765 8 1392 883 8 1393 1060 8 1394 1232 8 1395 834 8 1396 1145 8 1397 400 8 1398 801 8 1399 945 8 1400 889 8 1401 1146 8 1402 1468 9 1403 1666 9 1404 1230 9 1405 918 9 1406 1284 10 1407 410 10 1408 984 10 1409 860 10 1410 969 10 1411 721 10 1412 910 10 1413 941 10 1414 1227 10 1415 227 10 1416 1035 10 1417 1426 10 1418 431 10 1419 980 10 1420 930 10 1421 1321 10 1422 529 10 1423 337 10 1424 1145 10 1425 1331 10 1426 1655 10 1427 1454 10 1428 1700 10 1429 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