# Archive/proxy # Marine sediment #-------------------- # Contribution Date # Date: 2012-10-16 01:54:36 #-------------------- # Title # Study Name: MD95-2011 Norwegian Sea Marine sediment Diatoms #-------------------- # Investigators: #-------------------- # Description and Notes #-------------------- # Publication # Citation: Berner, K. S. and Koç, N. and Godtliebsen, F. and Divine, D. # Journal Name: Paleoceanography # Published Title: Holocene climate variability of the Norwegian Atlantic Current during high and low solar insolation forcing # Published Date: 2011 # DOI: 10.1029/2010PA002002 # Abstract: A high-resolution sediment core from the V\oring Plateau has been studied to document the centennial to millennial variability of the surface water conditions during the Holocene Climate Optimum (HCO) and the late Holocene period (LHP) in order to evaluate the effects of solar insolation on surface ocean climatology. Quantitative August summer sea surface temperatures (SSSTs) with a time resolution of 2–40 years are reconstructed by using three different diatom transfer function methods. Spectral- and scale-space methods are applied to the records to explore the variability present in the time series at different time scales. The SSST development in core MD95-2011 shows a delayed response to Northern Hemisphere maximum summer insolation at 11,000 years B.P. The record shows the maximum SSST of the HCO to be from 7.3 to 8.9 kyr B.P., which implies that the site was located in the regional warm water pool removed from the oceanic fronts and Arctic waters. Superimposed on the general cooling trend are higher-frequency variabilities at time scales of 80–120, 210–320, 320–640, and 640–1280 years. The climate variations at the time scale of 320–640 years are documented both for periods of high and low solar orbital insolation. We found evidence that the submillennial-scale mode of variability (640–900 years) in SSST evident during the LHP is directly associated with varying solar forcing. At the shorter scale of 260–450 years, the SSST during the LHP displays a lagged response to solar forcing with a phase-locked behavior indicating the existence of a feedback mechanism in the climate system triggered by variations in the solar constant as well as the role of the thermal inertia of the ocean. The abruptness of the cooling events in the LHP, especially pronounced during the onsets of the Holocene Cold Period I (approximately 2300 years B.P.) and the Little Ice Age (approximately 550 years B.P.), can be explained by a shutdown of deep convection in the Nordic Seas in response to negative solar insolation anomalies. These cooling events are on the order of 1.5°C. #---------------------- # Science Keywords: PAGES 2k Network, PAGES Arctic 2k, Arctic 2k, temperature, decadal resolution #-------------------- # Site Name # Region: North Atlantic # Country: Norwegian Sea # Northmost Latitude: 66.97 # Southmost Latitude: 66.97 # Eastmost Longitute: 7.64 # Westmost Longitute: 7.64 # Elevation: 0 #------------------ # Data Collection # Core Name: MD95-2011 # First Year: -4076.1 # Last Year: 1995.4 # Time Unit: AD #------------------ # Searchable Controlled Keywords # >paleocean>reconstruction>Sea Surface Temperature (C) #---------------- # Variables # age_AD Age (years AD) # sst Sea Surface Temperature (C) # age_AD sst 1995.4 10.2475 1991.1 9.93495 1985.1 10.3486 1979.9 10.8137 1975 10.3069 1970.1 10.1987 1965 10.6744 1960 10.4874 1955.2 10.4802 1950.6 10.4316 1946.4 10.3441 1942.6 10.1976 1939.2 9.94177 1936.2 10.2465 1933.7 10.3091 1931.8 10.5021 1930.3 9.71059 1928.9 10.1213 1927.2 10.6279 1924.6 10.3989 1920.7 10.1562 1915.2 10.3988 1908 9.97116 1899.3 9.81941 1889.2 10.4567 1877.8 10.0531 1865.2 10.6238 1851.6 10.1062 1837 10.5741 1821.5 10.1164 1805.3 10.6032 1788.5 10.5351 1771.3 10.3872 1753.6 10.3021 1735.6 10.3557 1717.5 9.98546 1699.4 10.2224 1681.3 10.3182 1663.4 10.1751 1645.8 10.5092 1628.5 10.1342 1611.9 9.60502 1595.8 10.2526 1580.5 9.93182 1566 10.1033 1552.4 10.1318 1539.5 9.90972 1527.3 9.62181 1515.8 10.1878 1504.9 9.61285 1494.6 9.8807 1484.9 10.2089 1475.6 10.0801 1466.7 10.0051 1458.2 9.97152 1450 9.80507 1442.2 9.30174 1434.6 10.0989 1427.1 9.66697 1419.8 9.79304 1414 9.78687 1409.7 10.1931 1405.3 9.49782 1401 9.99325 1396.6 10.0112 1392.1 9.57557 1387.7 9.79503 1383.1 10.3716 1378.5 10.7675 1373.9 10.3015 1369.2 10.7571 1364.5 10.9221 1359.6 10.6962 1354.7 10.4108 1349.8 10.3792 1344.7 10.6756 1339.6 10.2003 1329.2 10.7035 1323.8 10.0836 1318.3 10.1802 1312.8 10.2853 1307.1 9.73541 1301.4 10.6234 1295.5 10.3526 1289.5 10.5218 1283.4 10.1007 1277.2 10.3398 1270.9 10.9197 1264.5 9.97714 1257.9 10.3431 1251.2 10.4352 1244.4 10.4536 1237.5 10.2456 1230.4 10.458 1223.3 10.2323 1216 9.90654 1208.5 10.0018 1201 10.1752 1193.3 10.1555 1185.5 10.31 1177.6 9.97843 1169.5 9.92545 1161.3 10.0838 1153 10.2683 1144.5 10.2706 1135.9 10.2555 1127.2 10.2683 1118.4 10.2706 1109.5 10.4437 1100.4 10.6707 1091.2 10.5718 1082 10.636 1072.6 10.4771 1063.1 10.1984 1053.5 10.8871 1043.9 10.4754 1034.1 10.4251 1024.2 10.2876 1014.3 10.4069 1004.2 10.5756 994 10.9428 983.8 10.5078 973.4 10.3748 963 10.0874 952.4 10.5621 941.8 10.29 931.1 10.4755 920.2 10.8161 909.3 10.7187 898.3 11.2032 887.2 11.31 876 10.9428 864.7 10.6819 853.4 11.2742 841.9 10.5021 830.4 10.6746 818.8 10.7136 807.1 10.4963 795.3 10.7422 783.4 10.3953 771.5 10.3976 759.5 10.5862 747.4 10.0343 735.2 10.4764 722.9 10.0496 710.6 10.1461 698.2 10.1856 685.8 10.9432 673.3 10.2439 660.7 10.2711 648 10.5614 635.3 10.3516 622.6 10.038 609.8 10.4802 596.9 10.5782 584 10.6686 571.1 10.7675 558.1 10.4535 545.2 11.1143 532.1 10.4365 519.1 10.1557 506 10.4445 493 10.7043 479.9 10.6502 466.8 10.1643 453.8 10.5446 440.7 10.3205 427.7 10.3155 414.6 10.5336 401.6 10.5491 388.6 10.3853 375.7 10.6336 362.8 10.4685 349.9 10.3814 337.1 10.419 324.3 10.4213 311.6 10.5253 299 10.2192 286.4 10.4339 273.9 10.5301 261.4 10.6715 249.1 9.83745 236.8 10.4076 224.5 10.325 212.4 10.4571 200.3 9.73376 188.3 10.4793 176.3 10.5719 164.5 10.1528 152.7 10.4474 141 10.2335 129.3 10.6345 117.7 10.5028 106.2 10.1434 94.7 10.4129 83.3 10.5912 71.9 10.7858 60.6 10.0252 49.2 10.4125 38 10.1536 26.7 10.0339 15.5 10.6027 4.4 10.0681 -6.8 9.65882 -17.9 10.3951 -29.1 9.54885 -40.2 9.67012 -51.3 9.60315 -62.4 9.71098 -73.5 9.48452 -84.6 10.017 -95.7 9.73464 -106.8 9.91332 -118 10.1948 -129.1 10.0309 -140.2 9.83135 -151.4 10.0682 -162.5 9.67069 -207.3 9.94772 -218.5 9.62563 -229.7 9.60868 -240.9 10.0657 -252.2 10.0743 -263.5 10.2374 -274.7 9.57675 -286 10.2945 -297.4 10.6303 -308.7 10.1232 -320.1 10.3832 -331.5 10.5741 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