# AGASSIZ Ice Core
#-----------------------------------------------------------------------
#               World Data Center for Paleoclimatology, Boulder
#                                  and
#                     NOAA Paleoclimatology Program
#-----------------------------------------------------------------------
# NOTE: Please cite original reference when using these data,
# If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed
#
#
#
# Online_Resource: https://www.ncdc.noaa.gov/cdo/f?p=519:1:::::P1_STUDY_ID:2431
#
# Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24611
#
# Original_Source_URL: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/polar/agassiz/a77del18_1yr.txt
#
# Description/Documentation lines begin with #
# Data lines have no #
#
# Archive: Ice Cores
# --------------------
# Contribution_date
#	Date: 2015
# --------------------
# Title 
#	Study_Name: AGASSIZ Ice Core
#
# --------------------
# Investigators
#	Investigators: Fisher, D.A.; Koerner, R.M.; Reeh, N.
# --------------------
# Description_and_Notes
#	Description: 
#
# --------------------
# Publication
#	Authors: David A. Fisher, Roy M. Koerner, Niels Reeh
#	Published_Date_or_Year: 1995-03
#	Published_Title: Holocene climatic records from Agassiz Ice Cap, Ellesmere Island, NWT, Canada 
#	Journal_Name: The Holocene
#	Volume: 5
#	Edition: 	
#	Issue: 1 
#	Pages: 19-24
#	DOI: 10.1177/095968369500500103
#	Online_Resource: 
#	Full_Citation: 
#	Abstract: Four ice cores from the top of the Agassiz Ice Cap and down a flow line have been variously analysed for 8 (18O), ECM (solid conductivity) and ice-melt layer stratigraphy. Stratigraphic correlation of volcanic horizons is used to date the last 8000 years of the cores. The timescales at the Wisconsin/ Holocene transition are pinned at the new GRIP ice-core date. Both 8 and summer-melt records from cores A84 and A87 imply summer temperatures have decreased from 8000 BP to the present by about 2.0 degrees C. Differences in the various 8 series are explained in terms of local drift noise, excessive summer melt and ice flow originating from higher up the local dome where winter snow is scoured away. The present accumulation pattern along the flow line allows one to explain the smoothed differences in the delta records from 8000 BP to the present, but the massive summer melting between 8000 BP and the transition seems to have significantly altered the site and possibly introduced discontinuities. The massive summer melting in the early Holocene alters the volcanic acid (ECM) record in all the cores.
# --------------------
#	Authors: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G.J., Noone, D., Perkins, W.A., and E. Steig
#	Published_Date_or_Year: 2018
#	Published_Title: Additions to the last millennium reanalysis multi-proxy database
#	Journal_Name: Data Science Journal
#	Volume:
#	Edition:
#	Issue:
#	Pages:
#	Report_Number:
#	DOI:
#	Online_Resource:
#	Full_Citation: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G., J., Noone, D., Perkins, W.A., and E. Steig, submitted. Additions to the last millennium reanalysis multi-proxy database. Data Science Journal.
#	Abstract: Progress in paleoclimatology increasingly occurs via data syntheses. We describe additions to a collection prepared for use in paleoclimate state estimation, specifically the Last Millennium Reanalysis (LMR).  The 2290 additional series include 2152 tree ring chronologies and 138 other series.  They supplement the collection used previously and together form a database titled LMRdb 1.0.0. The additional data draws from lake core, ice core, coral, speleothem, and tree ring archives, using published data primarily from the NOAA Paleoclimatology archive and a set of tree ring width chronologies standardized from raw International Tree Ring Data Bank ring width series. In contrast to many previous paleo compilations, the data were not selected (screened) on the basis of their environmental correlation, multi-century length, or other attributes. The inclusion of proxies sensitive to moisture and other environmental variables expands their use in data assimilation.  A preliminary calibration using linear regression with mean annual temperature reveals characteristics of the proxy series and their relationship to temperature, as well as the noise and error characteristics of the records. The additional records are structured as individual files in the NOAA Paleoclimatology format and archived at NOAA Paleoclimatology (Anderson et al. 2018) and will continue to be improved and expanded as part of the LMR Project.  The additions represent a four-fold increase in the number of records available for assimilation, provide expanded geographic coverage, and add additional proxy variables.  Applications include data assimilation, proxy system model development, and paleoclimate reconstruction using climate field reconstruction and other methods.
#------------------
# Funding_Agency
#	Funding_Agency_Name: 
#	Grant: 
# --------------------
#	Funding_Agency_Name: National Science Foundation
#	Grant:AGS-1304263
#	Funding_Agency_Name: National Oceanic and Atmospheric Administration
#	Grant:NA14OAR4310176
#------------------
# Site_Information
#	Site_Name: Agassiz Ice Cap
#	Location: North America>Canada	
#	Country: Canada
#	Northernmost_Latitude: 80.25
#	Southernmost_Latitude: 80.25
#	Easternmost_Longitude: -72.983
#	Westernmost_Longitude: -72.983
#	Elevation: 1730 m
# --------------------
# Data_Collection
#	Collection_Name: 95Agas02
#	Earliest_Year: 973
#	Most_Recent_Year: 1972 
#	Time_Unit: y_ad
#	Notes: {"database":"LMR"} 
#
# --------------------
# Variables
#
# Data variables follow that are preceded by "##" in columns one and two.
# Data line variables format:  Variables list, one per line, shortname-tab-longname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) 
#
##age	age,,,years AD,,,,,N
##d18O	delta 18 oxygen,,,permil SMOW,,Ice Cores,,,N
#
# --------------------
# Data:
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing variables: NAN
#
age	d18O
1972	-27.69
1971	-28
1970	-28.11
1969	-27.8
1968	-27.73
1967	-29.02
1966	-28.5
1965	-27.94
1964	-27.11
1963	-26.52
1962	-26.24
1961	-26.73
1960	-26.31
1959	-26.17
1958	-26.21
1957	-26.66
1956	-26.84
1955	-28.68
1954	-28.47
1953	-27.01
1952	-27.85
1951	-29.72
1950	-29.02
1949	-28.53
1948	-28.54
1947	-29.29
1946	-28.55
1945	-27.62
1944	-27.17
1943	-27.13
1942	-26.78
1941	-26.5
1940	-26.81
1939	-27.69
1938	-27.86
1937	-27.5
1936	-27.17
1935	-27.28
1934	-27.28
1933	-28.1
1932	-28.38
1931	-28.46
1930	-28.56
1929	-28.62
1928	-29.55
1927	-29.55
1926	-30.11
1925	-29.69
1924	-27.6
1923	-27.44
1922	-27.35
1921	-27.93
1920	-27.95
1919	-27.99
1918	-28.06
1917	-28.32
1916	-29.24
1915	-29.28
1914	-29.31
1913	-29.44
1912	-29.34
1911	-29.13
1910	-28.78
1909	-28.61
1908	-29.63
1907	-29.75
1906	-30.01
1905	-29.22
1904	-28.89
1903	-29.07
1902	-29.13
1901	-29.2
1900	-27.99
1899	-27.6
1898	-26.96
1897	-27.16
1896	-27.34
1895	-26.71
1894	-26.78
1893	-27
1892	-27.89
1891	-28.29
1890	-28.9
1889	-28.38
1888	-27.83
1887	-27.36
1886	-27.33
1885	-27.54
1884	-27.72
1883	-27.85
1882	-28
1881	-28.1
1880	-28.28
1879	-28.51
1878	-28.57
1877	-28.28
1876	-28.4
1875	-28.55
1874	-28.91
1873	-28.84
1872	-28.48
1871	-28.18
1870	-28.23
1869	-28.66
1868	-28.47
1867	-28.46
1866	-28.72
1865	-28.77
1864	-28.83
1863	-29.14
1862	-28.9
1861	-28.64
1860	-26.96
1859	-27.32
1858	-27.77
1857	-28.95
1856	-29.19
1855	-29.07
1854	-28.49
1853	-28.23
1852	-28.53
1851	-29.1
1850	-29.79
1849	-29.84
1848	-29.82
1847	-29.56
1846	-29.51
1845	-29.45
1844	-29.35
1843	-28.86
1842	-28.36
1841	-28.12
1840	-28.22
1839	-28.39
1838	-28.38
1837	-28.33
1836	-28.25
1835	-28.36
1834	-28.24
1833	-28.25
1832	-28.57
1831	-28.96
1830	-28.85
1829	-28.68
1828	-28.48
1827	-28.69
1826	-28.81
1825	-28.84
1824	-28.67
1823	-28.41
1822	-28.1
1821	-27.91
1820	-27.95
1819	-28.28
1818	-28.38
1817	-28.39
1816	-28.29
1815	-29.17
1814	-29.39
1813	-29.22
1812	-28.7
1811	-28.45
1810	-28.59
1809	-28.97
1808	-29.42
1807	-29.75
1806	-29.58
1805	-29.44
1804	-29.25
1803	-29.03
1802	-28.82
1801	-28.28
1800	-28.05
1799	-28.07
1798	-28.29
1797	-28.76
1796	-29.06
1795	-28.99
1794	-28.67
1793	-28.13
1792	-27.49
1791	-27.42
1790	-27.81
1789	-28.35
1788	-28.94
1787	-29.32
1786	-28.08
1785	-27.39
1784	-27.37
1783	-27.91
1782	-28.13
1781	-28.27
1780	-28.33
1779	-28.17
1778	-28.34
1777	-28.49
1776	-28.46
1775	-28.53
1774	-28.42
1773	-28.2
1772	-28.08
1771	-28.57
1770	-28.92
1769	-28.91
1768	-28.96
1767	-28.73
1766	-28.34
1765	-28.11
1764	-28.09
1763	-28.14
1762	-28.29
1761	-28.81
1760	-28.93
1759	-29.03
1758	-29.33
1757	-29.09
1756	-28.75
1755	-28.24
1754	-28.52
1753	-29.15
1752	-29.84
1751	-30.43
1750	-30.76
1749	-30.17
1748	-29.19
1747	-27.9
1746	-28.63
1745	-29.21
1744	-29.73
1743	-30.38
1742	-31.01
1741	-31.51
1740	-31.28
1739	-30.19
1738	-29.5
1737	-28.93
1736	-28.36
1735	-28.44
1734	-28.63
1733	-29.15
1732	-29.46
1731	-29.7
1730	-29.92
1729	-29.6
1728	-29.62
1727	-29.79
1726	-29.96
1725	-29.66
1724	-29.31
1723	-28.9
1722	-28.95
1721	-28.93
1720	-28.55
1719	-28.44
1718	-28.52
1717	-28.81
1716	-29.32
1715	-29.39
1714	-29.39
1713	-29.72
1712	-29.81
1711	-29.81
1710	-29.53
1709	-29.28
1708	-29.16
1707	-29.09
1706	-28.76
1705	-28.45
1704	-28.07
1703	-27.86
1702	-28.19
1701	-28.57
1700	-29.55
1699	-29.71
1698	-29.89
1697	-30.41
1696	-30.36
1695	-30.31
1694	-30.15
1693	-30.14
1692	-30.14
1691	-30.2
1690	-30.02
1689	-29.86
1688	-29.48
1687	-29.29
1686	-29.15
1685	-29.13
1684	-29.39
1683	-29.52
1682	-29.52
1681	-29.24
1680	-29.18
1679	-29.3
1678	-29.88
1677	-30.2
1676	-30.58
1675	-29.53
1674	-29.6
1673	-30.09
1672	-30.32
1671	-30.1
1670	-29.65
1669	-29.92
1668	-29.46
1667	-28.57
1666	-28.35
1665	-28.39
1664	-28.54
1663	-28.94
1662	-29.09
1661	-29.24
1660	-29.34
1659	-29.44
1658	-29.65
1657	-29.94
1656	-29.66
1655	-27.71
1654	-27.42
1653	-27.29
1652	-27.88
1651	-28.42
1650	-28.92
1649	-28.6
1648	-29.05
1647	-29.73
1646	-29.39
1645	-29.23
1644	-29.05
1643	-29.3
1642	-29.69
1641	-30.43
1640	-30.95
1639	-30.56
1638	-29.21
1637	-28.77
1636	-28.53
1635	-28.24
1634	-28.25
1633	-28.2
1632	-27.96
1631	-27.95
1630	-27.97
1629	-28.15
1628	-28.23
1627	-28.3
1626	-28.24
1625	-28.17
1624	-28.08
1623	-28.55
1622	-28.72
1621	-28.92
1620	-28.33
1619	-28.03
1618	-27.61
1617	-27.61
1616	-27.61
1615	-27.67
1614	-27.86
1613	-28.14
1612	-28.04
1611	-28.07
1610	-28.26
1609	-28.15
1608	-28.07
1607	-27.46
1606	-27.7
1605	-28.02
1604	-27.34
1603	-27.27
1602	-27.64
1601	-28.1
1600	-28.44
1599	-28.13
1598	-27.45
1597	-26.71
1596	-28.19
1595	-28.82
1594	-29.71
1593	-29.25
1592	-28.81
1591	-27.71
1590	-27.52
1589	-27.51
1588	-28.75
1587	-28.65
1586	-28.56
1585	-28.43
1584	-28.77
1583	-29.48
1582	-29.23
1581	-29.05
1580	-28.5
1579	-28.69
1578	-28.85
1577	-28.46
1576	-28.47
1575	-28.56
1574	-28.84
1573	-28.95
1572	-28.98
1571	-28.77
1570	-28.55
1569	-28.31
1568	-28.25
1567	-28.19
1566	-27.68
1565	-27.34
1564	-28.05
1563	-28.29
1562	-28.76
1561	-28.24
1560	-27.98
1559	-27.58
1558	-27.86
1557	-28.3
1556	-28.26
1555	-28.26
1554	-28.28
1553	-28.07
1552	-27.98
1551	-28.38
1550	-28.38
1549	-28.39
1548	-28.21
1547	-28.2
1546	-28.22
1545	-28.23
1544	-28.25
1543	-28.39
1542	-28.85
1541	-29.35
1540	-30.11
1539	-29.99
1538	-29.23
1537	-29.09
1536	-29.01
1535	-30.07
1534	-30.07
1533	-30.07
1532	-28.55
1531	-27.93
1530	-27
1529	-27.22
1528	-27.46
1527	-28.44
1526	-28.7
1525	-29.05
1524	-28.74
1523	-28.49
1522	-28.82
1521	-28.92
1520	-29.13
1519	-28.56
1518	-28.15
1517	-27.78
1516	-27.92
1515	-28.47
1514	-29.21
1513	-29.72
1512	-30.19
1511	-30.24
1510	-30.26
1509	-30.28
1508	-30.3
1507	-28.8
1506	-28.47
1505	-28
1504	-27.74
1503	-27.55
1502	-28.16
1501	-28.71
1500	-29.68
1499	-29.77
1498	-29.81
1497	-29.92
1496	-29.6
1495	-29.27
1494	-29.7
1493	-29.84
1492	-30.06
1491	-28.86
1490	-28.11
1489	-27.6
1488	-27.56
1487	-27.52
1486	-27.48
1485	-27.51
1484	-28.95
1483	-29.44
1482	-30.22
1481	-29.07
1480	-28.64
1479	-28.39
1478	-28.35
1477	-28.29
1476	-27.9
1475	-27.67
1474	-26.72
1473	-26.64
1472	-26.52
1471	-26.95
1470	-27.07
1469	-26.74
1468	-26.75
1467	-26.76
1466	-27.1
1465	-27.29
1464	-29.53
1463	-29.15
1462	-28.39
1461	-27.95
1460	-27.68
1459	-27.44
1458	-27.52
1457	-27.83
1456	-28.14
1455	-28.4
1454	-28.04
1453	-28.02
1452	-28.08
1451	-27.71
1450	-27.53
1449	-27.83
1448	-28.28
1447	-28.91
1446	-29.2
1445	-29.26
1444	-29.11
1443	-28.93
1442	-28.76
1441	-28.1
1440	-27.98
1439	-27.91
1438	-27.92
1437	-27.92
1436	-27.98
1435	-28.11
1434	-28.45
1433	-29.14
1432	-29.58
1431	-29.28
1430	-28.79
1429	-27.56
1428	-27.28
1427	-27.24
1426	-27.81
1425	-27.77
1424	-27.73
1423	-27.56
1422	-27.91
1421	-28.52
1420	-29.25
1419	-29.47
1418	-29.56
1417	-29.64
1416	-29.69
1415	-28.61
1414	-28.49
1413	-28.33
1412	-28.4
1411	-28.34
1410	-28.02
1409	-27.09
1408	-26.44
1407	-27.41
1406	-28.17
1405	-29.44
1404	-28.66
1403	-28.23
1402	-27.2
1401	-27.09
1400	-26.99
1399	-27.67
1398	-28.29
1397	-29.85
1396	-29.71
1395	-29.63
1394	-29.59
1393	-29.51
1392	-29.36
1391	-29.06
1390	-28.89
1389	-28.27
1388	-28.87
1387	-29.7
1386	-29.43
1385	-29.38
1384	-29.59
1383	-29.21
1382	-28.8
1381	-28.25
1380	-27.92
1379	-26.82
1378	-27.49
1377	-28.15
1376	-28.96
1375	-29.11
1374	-28.95
1373	-28.76
1372	-28.55
1371	-28.79
1370	-28.85
1369	-28.92
1368	-28.58
1367	-28.24
1366	-28.14
1365	-28.19
1364	-28.38
1363	-27.86
1362	-27.49
1361	-27.85
1360	-27.98
1359	-28.24
1358	-27.74
1357	-27.5
1356	-28.04
1355	-27.73
1354	-27.16
1353	-27.46
1352	-27.64
1351	-28.91
1350	-29.09
1349	-29.4
1348	-29.77
1347	-29.92
1346	-30.05
1345	-30.61
1344	-31.49
1343	-30.24
1342	-29.66
1341	-26.91
1340	-27.44
1339	-28.4
1338	-29.12
1337	-29.48
1336	-28.76
1335	-28.4
1334	-27.55
1333	-27.68
1332	-27.77
1331	-28.53
1330	-28.8
1329	-29.56
1328	-29.53
1327	-29.5
1326	-28.82
1325	-28.61
1324	-28.09
1323	-27.82
1322	-27.43
1321	-28.1
1320	-28.39
1319	-29.04
1318	-28.94
1317	-28.6
1316	-28.34
1315	-28.12
1314	-27.83
1313	-27.74
1312	-27.42
1311	-27.36
1310	-27.28
1309	-27.53
1308	-27.61
1307	-27.57
1306	-27.55
1305	-27.52
1304	-27.34
1303	-27.27
1302	-27.78
1301	-28
1300	-28.52
1299	-28.92
1298	-29.17
1297	-29.16
1296	-29.21
1295	-29.38
1294	-29.24
1293	-29.11
1292	-28.73
1291	-28.56
1290	-27.84
1289	-27.95
1288	-28.12
1287	-28.54
1286	-28.75
1285	-27.73
1284	-27.95
1283	-28.83
1282	-28.72
1281	-28.61
1280	-27.94
1279	-27.75
1278	-27.34
1277	-27.46
1276	-27.71
1275	-27.78
1274	-27.83
1273	-27.7
1272	-27.6
1271	-26.98
1270	-27.58
1269	-28.63
1268	-28.76
1267	-28.84
1266	-28.24
1265	-28.43
1264	-29.39
1263	-29.73
1262	-29.98
1261	-29.73
1260	-29.58
1259	-29.24
1258	-29.25
1257	-29.25
1256	-28.4
1255	-28.56
1254	-28.97
1253	-29.41
1252	-29.65
1251	-29.3
1250	-29.43
1249	-29.71
1248	-29.3
1247	-29.08
1246	-28.57
1245	-28.66
1244	-28.9
1243	-28.21
1242	-27.8
1241	-26.98
1240	-27.13
1239	-27.64
1238	-27.68
1237	-27.7
1236	-27.56
1235	-27.74
1234	-28.49
1233	-28.47
1232	-28.45
1231	-28.97
1230	-29
1229	-28.45
1228	-28.72
1227	-29.1
1226	-28.71
1225	-28.56
1224	-28.9
1223	-29.03
1222	-29.34
1221	-29.42
1220	-29.47
1219	-28.94
1218	-28.65
1217	-27.54
1216	-28.1
1215	-28.81
1214	-28.85
1213	-28.86
1212	-28.87
1211	-28.55
1210	-27.65
1209	-27.51
1208	-27.38
1207	-27.65
1206	-27.75
1205	-28.29
1204	-28.64
1203	-29.38
1202	-28.72
1201	-28.24
1200	-27.81
1199	-27.73
1198	-27.8
1197	-27.84
1196	-27.88
1195	-29.08
1194	-29.52
1193	-30.27
1192	-30.03
1191	-29.82
1190	-29.54
1189	-29.22
1188	-28.33
1187	-28.02
1186	-27.8
1185	-27.61
1184	-27.58
1183	-27.52
1182	-27.51
1181	-27.5
1180	-26.51
1179	-26.83
1178	-27.68
1177	-27.64
1176	-27.62
1175	-27.12
1174	-27.08
1173	-27.02
1172	-26.8
1171	-26.66
1170	-26.56
1169	-26.62
1168	-26.79
1167	-28.15
1166	-29
1165	-29.93
1164	-30.03
1163	-30.12
1162	-29.41
1161	-28.85
1160	-28.11
1159	-27.91
1158	-27.47
1157	-27.4
1156	-27.32
1155	-27.84
1154	-28.1
1153	-29.37
1152	-29.23
1151	-29
1150	-29.57
1149	-29.86
1148	-28.91
1147	-28.52
1146	-27.44
1145	-27.63
1144	-27.79
1143	-27.98
1142	-28.03
1141	-28.15
1140	-28.05
1139	-27.87
1138	-28.11
1137	-28.22
1136	-28.09
1135	-28.14
1134	-28.37
1133	-29.02
1132	-29.72
1131	-29.31
1130	-29.16
1129	-28.37
1128	-28.48
1127	-28.78
1126	-28.09
1125	-27.73
1124	-28.77
1123	-28.39
1122	-27.82
1121	-27.31
1120	-27.18
1119	-27.38
1118	-27.43
1117	-27.47
1116	-27.63
1115	-27.68
1114	-27.77
1113	-27.73
1112	-27.71
1111	-28.59
1110	-28.81
1109	-29.21
1108	-28.91
1107	-28.75
1106	-28.25
1105	-27.96
1104	-27.54
1103	-27.95
1102	-28.11
1101	-28.34
1100	-27.97
1099	-27.49
1098	-27.79
1097	-27.93
1096	-28.44
1095	-28.57
1094	-28.74
1093	-28.65
1092	-28.61
1091	-28.47
1090	-28.32
1089	-28.14
1088	-28.15
1087	-28.14
1086	-28.04
1085	-28.25
1084	-28.53
1083	-28.1
1082	-27.97
1081	-28.35
1080	-28.03
1079	-27.46
1078	-27.42
1077	-27.4
1076	-27.18
1075	-27.25
1074	-27.41
1073	-27.62
1072	-27.76
1071	-28.29
1070	-28.46
1069	-28.93
1068	-29.48
1067	-30.04
1066	-29.39
1065	-29.19
1064	-28.99
1063	-29.01
1062	-29.04
1061	-28.41
1060	-28.11
1059	-27.73
1058	-27.89
1057	-28.5
1056	-28.96
1055	-29.4
1054	-29.57
1053	-29.56
1052	-28.41
1051	-28.2
1050	-27.8
1049	-27.32
1048	-27.08
1047	-26.73
1046	-27.1
1045	-28.56
1044	-28.8
1043	-29.07
1042	-29.27
1041	-29.35
1040	-28.06
1039	-27.94
1038	-27.63
1037	-27.49
1036	-27.33
1035	-27.35
1034	-27.36
1033	-28.51
1032	-28.63
1031	-28.88
1030	-28.31
1029	-27.65
1028	-27.3
1027	-27.14
1026	-27.07
1025	-27.09
1024	-27.23
1023	-27.49
1022	-27.91
1021	-27.39
1020	-27.04
1019	-27.39
1018	-27.42
1017	-26.77
1016	-26.82
1015	-26.96
1014	-27.29
1013	-27.63
1012	-28.14
1011	-28.36
1010	-28.35
1009	-28.39
1008	-28.5
1007	-28.78
1006	-28.97
1005	-29.21
1004	-29.12
1003	-28.88
1002	-28.13
1001	-27.66
1000	-27.1
999	-27.28
998	-27.88
997	-27.54
996	-27.33
995	-27.69
994	-27.82
993	-28.13
992	-28.19
991	-28.23
990	-27.78
989	-27.7
988	-27.63
987	-27.77
986	-27.9
985	-28.13
984	-27.97
983	-26.78
982	-26.86
981	-26.95
980	-27.77
979	-28.09
978	-28.69
977	-28.39
976	-27.85
975	-27.37
974	-27.12
973	-27.35