Continuous water vapor isotope ratios, Summit, Greenland, 2012-2014

The data set consists of water vapor stable isotope ratios (hydrogen and oxygen) at eight heights on from the surface to 50 meters above the surface collected approximately daily between June 2012 through June 2014 at Summit Station, Greenland (72 ºN, -38 ºW, 3209m). The data were collected as part...

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Bibliographic Details
Main Author: David Noone
Format: Dataset
Language:unknown
Published: Arctic Data Center 2018
Subjects:
Online Access:https://doi.org/10.18739/A2P55DG3P
Description
Summary:The data set consists of water vapor stable isotope ratios (hydrogen and oxygen) at eight heights on from the surface to 50 meters above the surface collected approximately daily between June 2012 through June 2014 at Summit Station, Greenland (72 ºN, -38 ºW, 3209m). The data were collected as part of the NSF funded project "Closing the Isotope Hydrology at Summit: Measurements of Source Regions, Precipitation and Post-deposition Processes". The purpose of the data set is to complement observations of isotopic composition of surface snow isotope measurements alongside ancillary measurements of meteorology, turbulence and hydrometeor microphysics. Calibration procedure is documented by Bailey et al., (2015) and data utilization example given by Berkelhammer et al., (2016). Bailey, A., Noone, D., Berkelhammer, M., Steen-Larsen, H. C., and Sato, P.: The stability and calibration of water vapor isotope ratio measurements during long-term deployments, Atmos. Meas. Tech., 8, 4521-4538, https://doi.org/10.5194/amt-8-4521-2015, 2015. M. Berkelhammer, D. Noone, HC Steen-Larsen, A. Bailey, C. Cox, M. O'Neill, D. Schneider, J. White and K. Steffen (2016) Surface-atmosphere decoupling limits accumulation at Summit, Greenland. Science Advances. doi: 10.1126/sciadv.1501704