datasheet1_Triple Water Vapour–Isotopologues Record from Chhota Shigri, Western Himalaya, India: A Unified Interpretation based on δ17O, δ18O, δD and Comparison to Meteorological Parameters.csv

• Main Authors: S. Ranjan, AL. Ramanathan, Tirumalesh Keesari, Virendra B. Singh, Naveen Kumar, Manish Pandey, Markus C. Leuenberger
• Format: Dataset
• Language: unknown
• Published: 2021
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; Water vapour; isotopologues; Himalaya; microclimate; moisture source; long range transport; Southern Ocean; Indian
• Online Access: https://doi.org/10.3389/feart.2020.599632.s001; https://figshare.com/articles/dataset/datasheet1_Triple_Water_Vapour_Isotopologues_Record_from_Chhota_Shigri_Western_Himalaya_India_A_Unified_Interpretation_based_on_17O_18O_D_and_Comparison_to_Meteorological_Parameters_csv/13615079

The objective of this study is to investigate and understand the source and transportation of water vapour in the western Himalayan region—that is still missing—using water vapour stable isotopologues and air mass trajectory diagnostics. We report the first-time triple oxygen isotopic compositions of water vapour from high altitude western Himalaya (Chhota Shigri, India) and compare them with meteorological conditions at the site of investigation as well as tracked backwards through the Lagrangian air mass trajectory diagnostics. A total of 21 water vapour samples were collected using a quantitative cryogenic method. δ 17 O and δ 18 O values show a significant correlation coefficient of 0.999 (p <0.01). The temporal variations of δ 17 O, δ 18 O, δD, D-excess and 17 O-excess are 1.2, 2.3, 17.3, 11.6 and 39‰ permeg, respectively. δ 17 O and δ 18 O exhibit significant (p < 0.05) diurnal variations along with meteorological parameters. Chhota Shigri vapour isotopic results show a clear difference in the 17 O-excess value compared to near the south Indian Ocean and the Southern Ocean regions, reflecting the influence of local moisture recycling at the continental site. NCEP/NCAR reanalyses show lower Specific Humidity during the sampling period (September, ending month of the Indian summer monsoon) favouring evaporative conditions which are further corroborated through the Lagrangian moisture diagnostics suggesting frequent moisture uptake and moisture loss in specific regions.