AO : fixed original citation to Watanabe

Column 'IC07KADF-chron-NA1', with variable name 'yearEnsemble', was added to the dataset

year (MAT49c994c4f7): interpretation3_scope: '' has been replaced by 'climate'

d18O (IC07KADF01A): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (IC07KADF01A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
year (MAT49c994c4f7): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MAT49c994c4f7): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'

d18O (IC07KADF01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC07KADF01A): interpretation1_variable: 'T' has been replaced by 'temperature'
d18O (IC07KADF01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC07KADF01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (IC07KADF01A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC07KADF01A): interpretation1_variable: 'T' has been replaced by 'temperature'
d18O (IC07KADF01A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC07KADF01A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (IC07KADF01A): paleoData_longName: '' has been replaced by 'AD'
year (MAT49c994c4f7): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT49c994c4f7): paleoData_longName: '' has been replaced by 'AD'

Watanabe, O., Jouzel, J., Johnsen, S., Parrenin, F., Shoji, H. and Yoshida, N.: Homogeneous climate variability across East Antarctica over the past three glacial cycles, Nature, 422(6931), 509–512, doi:10.1038/nature01525, 2003.

Igarashi, M., Nakai, Y., Motizuki, Y., Takahashi, K., Motoyama, H. and Makishima, K.: Dating of the Dome Fuji shallow ice core based on a record of volcanic eruptions from AD 1260 to AD 2001, Polar Science, 5(4), 411–420, doi:10.1016/j.polar.2011.08.001, 2011.

This verifies that the amount effect acts as an important control on seasonal-decadal scale variations in the isotopic composition of Everest precipitation. More specifically, precipitation increases during periods of more intense convective activity, resulting in more negative dD. Variations in convective activity (i.e., amount effect) and moisture source region related to changes in atmospheric circulation are the dominant controls on the isotopic composition of precipitation in this region (see auxiliary material).