Stable isotopes in precipitation (δ18O and δD) from Yadong and Pali, central Himalayas
Authors/Creators
- 1. State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China and Lanzhou University, Lanzhou 733000, China
- 2. State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
- 3. Department of Physical Geography and the Bolin Centre for Climate Change, Stockholm University, 106 91 Stockholm, Sweden
- 4. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101 China
Description
Metadata
The isotopic compositions of daily precipitation were measured at two stations, Yadong and Pali, in the central Himalayas. The precision for δ18O and δD is ±0.1‰ and ±0.4‰, respectively. The meteorological data, including the collection of precipitation amounts and surface air temperature, was obtained by the Institute of Tibetan Plateau Research, Chinese Academy of Sciences, China.
Stations
| Station | Latitude | Longitude | Altitude (m.a.s.l.) | Sampling period | Samples (n) |
| Yadong | 27° 29’ 40” N | 88° 55’ 01” E | 2945 | 2014-03-13 - 2015-07-18 | 125 |
| Pali | 27° 43’ 16” N | 89° 09’ 08” E | 4300 | 2014-03-18 - 2015-07-23 | 130 |
Variable definitions
| Description | Unit | Equipment | Additional description |
| Date time | − | − | − |
| Air temperature | Celsius (°C) | − | − |
| Precipitation | mm | − | − |
| Water vapour isotopic ratio (δ18O) | per mil | Picarro-2130i Liquid Water Isotope Analyzer | Normalized to V-SMOW |
| Water vapour isotopic ratio (δD) | per mil | Picarro-2130i Liquid Water Isotope Analyzer | Normalized to V-SMOW |
| Deuterium excess (d-excess) | per mil | d-excess=δD-8*δ18O |
Reference paper
Axelsson, J., Gao, J., Eckhardt, S., Cassiani, M., Chen, D. & Zhang, Q. (2023). A precipitation isotopic response in 2014-2015 to moisture transport changes in the central Himalayas. Journal of Geophysical Research: Atmospheres
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Additional details
Related works
- Is described by
- Working paper: 10.22541/essoar.167525247.77367925/v1 (DOI)