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Song, Zhaoyang; Latif, Mojib; Park, Wonsun; Zhang, Yuming (2020): δ18O and Model data for enhanced Greenland surface-temperature variability during the Last Glacial Maximum [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.922864

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Abstract:
Stable oxygen isotope records from central Greenland suggest disproportionally large long-term surface-air temperature (SAT) variability during the last glacial maximum (LGM) relative to preindustrial times. Large perturbations in mean atmospheric circulation and its variability forced by extensive Northern Hemisphere ice sheet coverage has been suggested as cause for the enhanced Greenland SAT variability. Here, we assess the factors driving Greenland SAT variability during the LGM by means of dedicated climate model simulations and find remote forcing from the Pacific of critical importance. Atmospheric teleconnections from the Interdecadal Pacific Oscillation (IPO), a multidecadal oscillation of sea-surface temperature in the Pacific Ocean, strongly intensify under LGM conditions, driving enhanced surface wind variability over Greenland, which in turn amplifies SAT variability by anomalous atmospheric heat transport. A major role of the IPO in forcing Greenland SAT variability also is supported by a number of models from the Paleoclimate Modelling Intercomparison Project Phase III.
Keyword(s):
LGM
Supplement to:
Song, Zhaoyang; Latif, Mojib; Park, Wonsun; Zhang, Yuming (2020): Interdecadal Pacific Oscillation Drives Enhanced Greenland Surface Temperature Variability During the Last Glacial Maximum. Geophysical Research Letters, 47(23), https://doi.org/10.1029/2020GL088922
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Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DescriptionDescriptionSong, Zhaoyang
Binary ObjectBinarySong, Zhaoyang
Binary Object (File Size)Binary (Size)BytesSong, Zhaoyang
Binary Object (Media Type)Binary (Type)Song, Zhaoyang
Size:
26 data points

Data

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Binary (Size) [Bytes]

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Power spectrum calculated from the North Greenland Ice Core Project (NGRIP) and the red noise estimated from the first-order Markov modelFig_1a_NGRIP_Spectrum.nc5.3 kBytesapplication/x-netcdf
Power spectrum of Greenland surface air temperature calculated from the KCM PI and LGM experiments and the red noise estimated from the first-order Markov modelFig_1b_GR_T2m_Spectrum.nc201.5 kBytesapplication/x-netcdf
Power spectrum of Greenland surface air temperature calculated from the KCM restoring experiments and the red noise estimated from the first-order Markov modelFig_1c_Res_EXP_GR_T2m_Spectrum.nc60.2 kBytesapplication/x-netcdf
Regression of the global surface air temperature on the Greenland surface air temperature from the KCM PI and LGM experimentsFig_2ab_Global_T2m_regress_GR_T2m.nc321.7 kBytesapplication/x-netcdf
Cross spectrum of Greenland surface air temperature and tripole Interdecadal Pacific Oscillation Index (IPO) from the KCM PI and LGM experimentsFig_2cdef_GR_T2m_IPO_Cross_Spectrum.nc47.6 kBytesapplication/x-netcdf
Regression of 300 hPa geopotential height on the IPO index from the KCM PI and LGM experimentsFig_3ab_Geopoth_300hPa_regress_IPO.nc321.7 kBytesapplication/x-netcdf
Regression of sea level pressure (SLP) on the IPO index from the KCM PI and LGM experimentsFig_3cd_SLP_regress_IPO.nc258 kBytesapplication/x-netcdf
Regression of 700 hPa zonal wind on the IPO index from the KCM PI and LGM experimentsFig_3ef_Uwnd_700hPa_regress_IPO.nc257.9 kBytesapplication/x-netcdf
Regression of 700 hPa meridional wind on the IPO index from the KCM PI and LGM experimentsFig_3ef_Vwnd_700hPa_regress_IPO.nc257.9 kBytesapplication/x-netcdf
Regression of Eliassen-Palm flux on the IPO index from the KCM PI and LGM experimentsFig_3gh_EPFlux_regress_IPO.nc27.2 kBytesapplication/x-netcdf
Regression of Greenland surface air temperature on the IPO index from the KCM PI and LGM experimentsFig_3ij_T2m_regress_IPO.nc258.1 kBytesapplication/x-netcdf
Regression of Northern Hemisphere sea ice concentration on the IPO index from the KCM PI and LGM experimentsFig_3kl_SIC_regress_IPO.nc1.2 MBytesapplication/x-netcdf
Response of Greenland surface air temperature simulated in the stand-alone atmospheric simulationsFig_4_AGCM_GR_T2m_Response.nc27.4 kBytesapplication/x-netcdf