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Title: Variability in observed stable water isotopes in snowpack across a mountainous watershed in Colorado

Journal Article · · Hydrological Processes
DOI:https://doi.org/10.1002/hyp.14653· OSTI ID:1884783
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3]; ORCiD logo [4]; ORCiD logo [5]; ORCiD logo [5]; ORCiD logo [5]; ORCiD logo [4]; ORCiD logo [4]; ORCiD logo [4]
  1. Desert Research Inst. (DRI), Reno, NV (United States)
  2. National Snow and Ice Data Center, Boulder, CO (United States)
  3. Princeton Univ., NJ (United States)
  4. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
  5. Rocky Mountain Biological Lab., Gothic, CO (United States)

Abstract Isotopic information from 81 snowpits was collected over a 5‐year period in a large, Colorado watershed. Data spans gradients in elevation, aspect, vegetation, and seasonal climate. They are combined with overlapping campaigns for water isotopes in precipitation and snowmelt, and a land‐surface model for detailed estimates of snowfall and climate at sample locations. Snowfall isotopic inputs, describe the majority of δ 18 O snowpack variability. Aspect is a secondary control, with slightly more enriched conditions on east and north facing slopes. This is attributed to preservation of seasonally enriched snowfall and vapour loss in the early winter. Sublimation, expressed by decreases in snowpack d‐excess in comparison to snowfall contributions, increases at low elevation and when seasonal temperature and solar radiation are high. At peak snow accumulation, post‐depositional fractionation appears to occur in the top 25 ± 14% of the snowpack due to melt‐freeze redistribution of lighter isotopes deeper into the snowpack and vapour loss to the atmosphere during intermittent periods of low relative humidity and high windspeed. Relative depth of fractionation increases when winter daytime temperatures are high and winter precipitation is low. Once isothermal, snowpack isotopic homogenization and enrichment was observed with initial snowmelt isotopically depleted in comparison to snowpack and enriching over time. The rate of δ 18 O increase (d‐excess decrease) in snowmelt was 0.02‰ per day per 100‐m elevation loss. Isotopic data suggests elevation dictates snowpack and snowmelt evolution by controlling early snow persistence (or absence), isotopic lapse rates in precipitation and the ratio of energy to snow availability. Hydrologic tracer studies using stable water isotopes in basins of large topographic relief will require adjustment for these elevational controls to properly constrain stream water sourcing from snowmelt.

Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
Grant/Contract Number:
AC02-05CH11231
OSTI ID:
1884783
Alternate ID(s):
OSTI ID: 1885619
Journal Information:
Hydrological Processes, Vol. 36, Issue 8; ISSN 0885-6087
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English

References (55)

On Shear-Driven Ventilation of Snow journal November 2007
Spatial and Temporal Variability of Snow Isotopic Composition on Mt. Zugspitze, Bavarian Alps, Germany journal November 2018
Isotopic variation of snow cover and streamflow in response to changes in canopy structure in a snow-dominated mountain catchment journal January 2008
Input data processing tools for the integrated hydrologic model GSFLOW journal November 2018
Quantifying the effects of vegetation structure on snow accumulation and ablation in mixed-conifer forests: THE EFFECTS OF VEGETATION STRUCTURE ON SNOW IN MIXED-CONIFER FORESTS journal October 2014
Early melt season snowpack isotopic evolution in the Tarfala valley, northern Sweden journal January 2013
Streamflow partitioning and transit time distribution in snow-dominated basins as a function of climate journal March 2019
Representing spatial variability of snow water equivalent in hydrologic and land-surface models: A review: REPRESENTING SPATIAL VARIABILITY OF SWE IN MODELS journal July 2011
Isotopic evidence for lateral flow and diffusive transport, but not sublimation, in a sloped seasonal snowpack, Idaho, USA journal April 2016
Influence of sublimation on stable isotope records recovered from high-altitude glaciers in the tropical Andes journal October 2001
Spatial analysis of the intra-annual variation of precipitation isotope ratios and its climatological corollaries: PRECIPITATION ISOTOPIC SEASONALITY journal March 2008
Potential impacts of a warming climate on water availability in snow-dominated regions journal November 2005
Use of Water Isotopes in Hydrological Processes journal August 2020
The modular modeling system (MMS) — The physical process modeling component of a database-centered decision support system for water and power management journal July 1996
Isotopes in the Water Cycle: Regional- to Global-Scale Patterns and Applications journal May 2019
Isotopic evolution of a seasonal snowpack and its melt journal March 2001
A Global Perspective on Local Meteoric Water Lines: Meta‐analytic Insight Into Fundamental Controls and Practical Constraints journal August 2019
Stable isotopes in precipitation journal January 1964
Post-depositional modification of stable water isotopes in winter snowpacks in the Canadian Rocky Mountains journal January 2008
Persistence and Plasticity in Conifer Water‐Use Strategies journal February 2020
Factors controlling seasonal groundwater and solute flux from snow-dominated basins journal June 2018
Isotopic exchange between snow and atmospheric water vapor: Estimation of the snowmelt component of groundwater recharge in the southwestern United States journal January 2006
Environmental Isotope Studies of an Alpine Snowpack journal August 1981
Challenges in Building an End-to-End System for Acquisition, Management, and Integration of Diverse Data From Sensor Networks in Watersheds: Lessons From a Mountainous Community Observatory in East River, Colorado journal January 2019
Understanding snow hydrological processes through the lens of stable water isotopes journal July 2018
Persistent wind-induced enhancement of diffusive CO 2 transport in a mountain forest snowpack journal January 2011
Efficiency of the Summer Monsoon in Generating Streamflow Within a Snow‐Dominated Headwater Basin of the Colorado River journal December 2020
Mountain hydrology of the western United States: MOUNTAIN HYDROLOGY OF THE WESTERN US journal August 2006
Deuterium variations in an annual snowpack journal February 1970
Isotopic composition of precipitation in a topographically steep, seasonally snow-dominated watershed and implications of variations from the global meteoric water line journal August 2016
The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes journal December 2018
The Effect of Turbulence on Drifting Snow Sublimation journal October 2019
Seasonal Deuterium Excess Variations of Precipitation at Summit, Greenland, and their Climatological Significance journal January 2019
Is Evaporation an Important Component in High Alpine Hydrology? journal August 1981
Global Isotope Hydrogeology―Review journal July 2019
PRMS-IV, the precipitation-runoff modeling system, version 4 report January 2015
Annual variation in event-scale precipitation δ2H at Barrow, AK, reflects vapor source region journal January 2017
Spatial variation of snowmelt and sublimation in a high-elevation semi-desert basin of western Canada journal August 2009
On the importance of sublimation to an alpine snow mass balance in the Canadian Rocky Mountains journal January 2010
Stable isotope compositions of precipitation from Gunnison, Colorado 2007–2016: implications for the climatology of a high-elevation valley journal July 2019
Influence of the Depth Hoar Layer of the Seasonal Snow Cover on the Ground Thermal Regime journal July 1996
Stable isotopes in mineralogy journal January 1977
Difficulties in Determining Snowpack Sublimation in Complex Terrain at the Macroscale journal January 2016
The Importance of Snow Sublimation on a Himalayan Glacier journal August 2018
Modeling the isotopic evolution of snowpack and snowmelt: Testing a spatially distributed parsimonious approach journal July 2017
Sub-Hourly Variability of Stable Isotopes in Precipitation in the Marginal Zone of East Asian Monsoon journal July 2020
A Model for Deuterium and Oxygen 18 Isotope Changes During Evergreen Interception of Snowfall journal March 1995
Sublimation from a seasonal snowpack at a continental, mid-latitude alpine site journal September 1999
A distributed model of blowing snow over complex terrain journal October 1999
Snow Temperature Changes within a Seasonal Snowpack and Their Relationship to Turbulent Fluxes of Sensible and Latent Heat journal February 2014
Terrestrial water fluxes dominated by transpiration: Comment journal May 2014
Isotope variations in a Sierra Nevada snowpack and their relation to meltwater journal March 2002
Isotopic evolution of a seasonal snowcover and its melt by isotopic exchange between liquid water and ice journal February 2010
Seasonality of stable isotope composition of atmospheric water input at the southern slopes of Mt. Kilimanjaro, Tanzania journal September 2017
How isotopic fractionation of snowmelt affects hydrograph separation journal January 2002

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