# Trouet et al. 2009 NAO Reconstruction
#----------------------------------------------------------------------- 
#               World Data Service for Paleoclimatology, Boulder 
#                                  and 
#                     NOAA Paleoclimatology Program 
#----------------------------------------------------------------------- 
# Template Version 4.0
# Encoding: UTF-8
# NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available),
# and date accessed when using these downloaded data. If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed.
#
# NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/8713
#   Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata.
#
# Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-recon-8713.json
#   Study_Level_JSON_Description: JSON metadata of this file's parent study, which includes all study metadata.
#
# Data_Type: Climate Reconstructions
#
# Dataset_DOI:
#
# Science_Keywords: Atmospheric and Oceanic Circulation Patterns Reconstruction
#-------------------
# Resource_Links
#
# Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/reconstructions/nao-trouet2009-noaa.txt
#   Data_Download_Description: NOAA Template File; North Atlantic Oscillation Data
#
# Original_Source_URL: 
#   Original_Source_Description: 
#
#-------------------
# Contribution_Date
#   Date: 2009-04-01
#-------------------
# File_Last_Modified_Date
#   Date: 2022-03-30
#-------------------
# Title
#   Study_Name: Trouet et al. 2009 NAO Reconstruction
#-------------------
# Investigators
#   Investigators: Trouet, V.; Esper, J.; Graham, N.E.; Baker, A.; Scourse, J.D.; Frank, D.C.
#-------------------
# Description_Notes_and_Keywords
#   Description: Winter NAO Reconstruction 1049-1995 AD.  Decadal scale variations in a speleothem-based precipitation proxy from Scotland and a tree-ring based drought proxy from Morocco reflect quasi-regular occurrences of contrasting precipitation regimes over the Millennium.  These proxy records are located centrally in the opposing poles of North Atlantic Oscillation (NAO) driven precipitation regimes. Analogous to the instrumental based NAO index, we combined both records to develop a near millennium-long (1049-1995) record of winter NAO (wNAO).  A 30-year smoothing spline was applied to both proxy series and they were normalized over the common period before their residual was calculated.  Extreme phases in the difference record (Scotland minus Morocco) corresponded to typical wNAO related geopotential height and precipitation patterns over Europe over the last three centuries.  Low frequency NAO phases over the 20th century are well captured in the proxy record, which correlates reasonably well with instrumental wNAO index time series.  On longer time-scales, the multidecadal variations in our wNAO reconstruction are similar to the ones found in previous NAO reconstructions.  Our wNAO record, however, is 350 years longer than the currently longest reconstructions and extends into the Medieval Climate Anomaly (MCA), for which a persistent positive mode is reconstructed. 
#-------------------
# Publication
#   Authors: Trouet, V., J. Esper, N.E. Graham, A. Baker, J.D. Scourse, and D.C. Frank
#   Journal_Name: Science
#   Published_Title: Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly.
#   Published_Date_or_Year: 2009-04-03
#   Volume: 324
#   Issue: 
#   Pages: 78-80
#   Report_Number: 
#   DOI: 10.1126/science.1166349
#   Full_Citation: 
#   Abstract: The Medieval Climate Anomaly (MCA) was the most recent pre-industrial era warm interval of European climate, yet its driving mechanisms remain uncertain. We present here a 947-year-long multidecadal North Atlantic Oscillation (NAO) reconstruction and find a persistent positive NAO during the MCA. Supplementary reconstructions based on climate model results and proxy data indicate a clear shift to weaker NAO conditions into the Little Ice Age (LIA). Globally distributed proxy data suggest that this NAO shift is one aspect of a global MCA-LIA climate transition that probably was coupled to prevailing La Nina-like conditions amplified by an intensified Atlantic meridional overturning circulation during the MCA.
#-------------------
# Funding_Agency
#   Funding_Agency_Name: European Commission MILLENNIUM Integrated Project
#   Grant_Number: 017008
#-------------------
# Funding_Agency
#   Funding_Agency_Name: Swiss National Science Foundation through the National Centre for Competence in Climate Research (NCCR-Climate)
#   Grant_Number: 
#-------------------
# Funding_Agency
#   Funding_Agency_Name: National Oceanic and Atmospheric Administration (NOAA)
#   Grant_Number: NA06OA-R4310120
#-------------------
# Funding_Agency
#   Funding_Agency_Name: Royal Society-Leverhulme Trust 
#   Grant_Number: Senior Research Fellowship
#-------------------
# Site_Information
#   Site_Name: North Atlantic Oscillation
#   Location: North Atlantic Ocean
#   Northernmost_Latitude: 65
#   Southernmost_Latitude: 38
#   Easternmost_Longitude: -10
#   Westernmost_Longitude: -50
#   Elevation_m: 
#-------------------
# Data_Collection
#   Collection_Name: nao_Trouet2009b
#   First_Year: 1049
#   Last_Year: 1995
#   Time_Unit: CE
#   Core_Length_m: 
#   Parameter_Keywords: reconstructions
#   Notes: 
#-------------------
# Chronology_Information
#   Chronology:
#-------------------
# Variables 
#
# PaST_Thesaurus_Download_Resource:  https://www.ncdc.noaa.gov/paleo/skos/past-thesaurus.rdf
#   PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format.
#
# Variables format: shortname <tab> what,material,error,units,seasonality,data_type,detail,method, C(har) or N(umeric) data,additional information
#
## age	age,,,year Common Era,,climate reconstructions;speleothems;tree ring,,,N,
## nao	North Atlantic Oscillation Index,,,dimensionless,winter,climate reconstructions;speleothems;tree ring,,,N,
#
#-------------------------------
# Data: 
# Missing_Values: NA
age	nao
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1068	1.0112
1069	1.0932
1070	1.1712
1071	1.2456
1072	1.3146
1073	1.3758
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1075	1.4832
1076	1.5471
1077	1.6245
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1079	1.8234
1080	1.9419
1081	2.0723
1082	2.2072
1083	2.3397
1084	2.4623
1085	2.5663
1086	2.6436
1087	2.69
1088	2.7057
1089	2.6929
1090	2.6545
1091	2.596
1092	2.5244
1093	2.4481
1094	2.3721
1095	2.3039
1096	2.2533
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1098	2.2226
1099	2.2418
1100	2.281
1101	2.3328
1102	2.3875
1103	2.4329
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1111	2.0793
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1122	2.4364
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1124	2.4158
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1132	1.5555
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1137	1.4079
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1149	2.3364
1150	2.3719
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1155	2.626
1156	2.6782
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1756	-1.0514
1757	-1.187
1758	-1.326
1759	-1.4815
1760	-1.6664
1761	-1.8723
1762	-2.0775
1763	-2.254
1764	-2.3827
1765	-2.4582
1766	-2.4818
1767	-2.4613
1768	-2.4077
1769	-2.3346
1770	-2.2534
1771	-2.1707
1772	-2.0854
1773	-1.9932
1774	-1.892
1775	-1.7823
1776	-1.6723
1777	-1.5668
1778	-1.4681
1779	-1.3759
1780	-1.299
1781	-1.2495
1782	-1.2349
1783	-1.2515
1784	-1.287
1785	-1.3197
1786	-1.3255
1787	-1.2871
1788	-1.199
1789	-1.0671
1790	-0.91
1791	-0.7441
1792	-0.5803
1793	-0.4244
1794	-0.2827
1795	-0.1622
1796	-0.0684
1797	-0.0016
1798	0.0427
1799	0.0716
1800	0.0935
1801	0.1144
1802	0.1364
1803	0.1626
1804	0.1957
1805	0.2326
1806	0.2652
1807	0.2886
1808	0.3033
1809	0.3091
1810	0.3047
1811	0.2914
1812	0.2725
1813	0.2556
1814	0.2532
1815	0.2762
1816	0.3279
1817	0.4046
1818	0.496
1819	0.5921
1820	0.6825
1821	0.7544
1822	0.7968
1823	0.8047
1824	0.7754
1825	0.708
1826	0.6092
1827	0.4884
1828	0.3498
1829	0.197
1830	0.0383
1831	-0.1187
1832	-0.2672
1833	-0.3989
1834	-0.5096
1835	-0.598
1836	-0.6591
1837	-0.6907
1838	-0.6946
1839	-0.6814
1840	-0.6641
1841	-0.6554
1842	-0.6692
1843	-0.7115
1844	-0.7815
1845	-0.8689
1846	-0.9564
1847	-1.0291
1848	-1.0777
1849	-1.0926
1850	-1.0706
1851	-1.0167
1852	-0.9329
1853	-0.821
1854	-0.6834
1855	-0.5224
1856	-0.3401
1857	-0.1418
1858	0.0632
1859	0.2617
1860	0.4417
1861	0.5967
1862	0.7207
1863	0.808
1864	0.8601
1865	0.8814
1866	0.8784
1867	0.8588
1868	0.828
1869	0.7925
1870	0.7599
1871	0.7391
1872	0.7357
1873	0.7515
1874	0.7839
1875	0.8276
1876	0.8823
1877	0.9425
1878	0.9976
1879	1.0384
1880	1.0636
1881	1.071
1882	1.0527
1883	1.0031
1884	0.9282
1885	0.8415
1886	0.7565
1887	0.6836
1888	0.6303
1889	0.6057
1890	0.6128
1891	0.6479
1892	0.7012
1893	0.7619
1894	0.8253
1895	0.8889
1896	0.9473
1897	0.9923
1898	1.0164
1899	1.0189
1900	1.0026
1901	0.9732
1902	0.9388
1903	0.9044
1904	0.8731
1905	0.8471
1906	0.8295
1907	0.8278
1908	0.8466
1909	0.8858
1910	0.9419
1911	1.0115
1912	1.091
1913	1.1749
1914	1.2546
1915	1.3208
1916	1.3642
1917	1.377
1918	1.3539
1919	1.2935
1920	1.2018
1921	1.0902
1922	0.9713
1923	0.8549
1924	0.7473
1925	0.6504
1926	0.5617
1927	0.4793
1928	0.407
1929	0.3452
1930	0.2879
1931	0.2262
1932	0.1468
1933	0.0401
1934	-0.0985
1935	-0.2642
1936	-0.4476
1937	-0.6383
1938	-0.8275
1939	-1.0019
1940	-1.1457
1941	-1.2441
1942	-1.2901
1943	-1.2877
1944	-1.2511
1945	-1.1999
1946	-1.1511
1947	-1.1109
1948	-1.0838
1949	-1.0765
1950	-1.0961
1951	-1.1434
1952	-1.2118
1953	-1.2956
1954	-1.3863
1955	-1.4761
1956	-1.5651
1957	-1.6637
1958	-1.7825
1959	-1.9251
1960	-2.0855
1961	-2.249
1962	-2.399
1963	-2.5176
1964	-2.5896
1965	-2.6075
1966	-2.5685
1967	-2.4754
1968	-2.3332
1969	-2.1504
1970	-1.9431
1971	-1.7279
1972	-1.5148
1973	-1.3044
1974	-1.086
1975	-0.8459
1976	-0.5723
1977	-0.2575
1978	0.0972
1979	0.4825
1980	0.878
1981	1.2547
1982	1.585
1983	1.8528
1984	2.0496
1985	2.1767
1986	2.2438
1987	2.2667
1988	2.2634
1989	2.2548
1990	2.2591
1991	2.289
1992	2.3501
1993	2.4389
1994	2.5465
1995	2.6641