GNIP data for Groennedal and Prins Christians Sund, near the study site

Groennedal: 61.22°N, 48.12°W, 27 m asl; Prins Christians Sund: 60.03°N 43.12°W, 76 m asl

d2H (LS13BAFL01A): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS13BAFL01B): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS13BAFL01C): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS13BAFL01D): interpretation4_scope: '' has been replaced by 'isotope'

year (MAT27bb9b76f9): The paleoData_values have changed

Column 'addR1tI1yBfbKHFmvtxC', with variable name 'depth', was added to the dataset
Column 'addRivwII5y8fTGSVV9K', with variable name 'depth', was added to the dataset
Column 'addRMXCIODnyFZ6nxk1f', with variable name 'age.rangeHigh', was added to the dataset
Column 'addRrbED35eFB5bnaXFO', with variable name 'age', was added to the dataset
Column 'addRvK3LI9PO95IpDB1c', with variable name 'age.rangeLow', was added to the dataset
Column 'addRvkKBH3jOnOwTOQfD', with variable name 'ageEnsemble', was added to the dataset
Column 'LS13BAFL-chron-NA1', with variable name 'depth', was added to the dataset
Column 'LS13BAFL-chron-NA2', with variable name 'age.rangeLow', was added to the dataset
Column 'LS13BAFL-chron-NA3', with variable name 'age.rangeHigh', was added to the dataset
Column 'LS13BAFL-chron-NA4', with variable name 'age', was added to the dataset

Balascio, N. L. , DAndrea, W. J. , Bradley, R. S. , Perren, B. B.

Biogeochemical evidence for hydrologic changes during the Holocene in a lake sediment record from southeast Greenland

Balascio, N. L., D’Andrea, W. J., Bradley, R. S. and Perren, B. B.: Biogeochemical evidence for hydrologic changes during the Holocene in a lake sediment record from southeast Greenland, The Holocene, 23(10), 1428–1439, doi:10.1177/0959683613493938, 2013.

ASE350, HP 6890 GC, Finnigan MAT Delta+ XL mass spectrometer

dDprecip reflects Australasian monsoon strength based on modern precipitation isotope data from nearby station (Bali). "At Bali, the closest isotopic monitoring site to Lake Lading, over 80% of precipitation measured from July 2003 to June 2006 fell between October and March (61% during Novembera€“February), coinciding with the southernmost extension of the ITCZ associated with summer intensification of the Australasian monsoon (Figure 1c). The weighted Octo- bera€“March average dDprecip during that time period was 18.72%, similar to the weighted annual (Julya€“June) average of 20.42%, reflecting the strong control of wet season dDprecip on the annual average dDprecip [Kurita et al., 2009]. While large-scale changes in atmospheric circulation could certainly cause the relationship between precipitation amount and dDprecip to vary, these modern observations indicate that dDprecip reflects Australasian monsoon strength."