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Coal Creek -CO - Significant stream chemistry response to temperature variations in a high-elevation mountain watershed
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Created: | Oct 27, 2022 at 2:40 a.m. | |
Last updated: | Jan 26, 2023 at 9:26 p.m. | |
Citation: | See how to cite this resource | |
Content types: | Single File Content |
Sharing Status: | Public |
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Views: | 2311 |
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Abstract
High-elevation mountain regions, central to global freshwater supply, are experiencing more rapid warming than low-elevation locations. High-elevation streams are therefore potentially critical indicators for earth system and water chemistry response to warming. Here we present concerted hydroclimatic and biogeochemical data from Coal Creek, Colorado in the central Rocky Mountains at elevations of 2700 to 3700 m, where air temperatures have increased by about 2 °C since 1980. We analyzed water chemistry every other day from 2016 to 2019. Water chemistry data indicate distinct responses of different solutes to inter-annual hydroclimatic variations. Specifically, the concentrations of solutes from rock weathering are stable inter-annually. Solutes that are active in soils, including dissolved organic carbon, vary dramatically, with double to triple peak concentrations occurring during snowmelt and in warm years. We advocate for consistent and persistent monitoring of high elevation streams to record early glimpse of earth surface response to warming.1) Coal Creek stream were sampled and measured to answer the question if there is a significant stream chemistry response to climate change in high-elevation watershed2) The file contains data regarding discharge, water temperature and stream chemistry data for 2016-2019 year. Stream chemistry includes dissolved organic and inorganic carbon, chloride, nutrients, cations.
The data collection efforts were carried out by the DOE-funded "Advancing a Watershed Hydro-Biogeochemical Theory: Linking Water Travel Time and Reaction Rates Under Changing Climate" project and Watershed Function SFA.
Subject Keywords
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The content of this resource is similar to | Barnard, H., N. Hornslein, M. Schiff (2023). Water Chemistry - (GG1, GG2-1, 2, 3, 4, 5, 6 & SW0) -- Gordon Gulch -- (2020-ongoing), HydroShare, http://www.hydroshare.org/resource/6af194de17d04fcbbff49e3f2d3bf8c1 |
The content of this resource is similar to | Zhi, W., L. Li, W. Dong, W. Brown, J. Kaye, C. Steefel, K. Williams (2022). Coal Creek -CO - Distinct Source Water Chemistry Shapes Contrasting Concentration Discharge Patterns, HydroShare, http://www.hydroshare.org/resource/24b834aab72743db899b99404b48cb68 |
The content of this resource is similar to | Bush, S., H. R. Barnard, M. Schiff, N. Hornslein (2023). DWCZ - CO - Manitou Experimental Forest, Hotel Gulch - Water Chemistry - (DWCZ-MEF-HG-GW-SW-Array-SBush) - (2018-2021), HydroShare, http://www.hydroshare.org/resource/3c831dbc381d41a290f3d0cacdf4a8a4 |
Title | Owners | Sharing Status | My Permission |
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DWCZ CO - Coal Creek (CC) | Eric Parrish | Public & Shareable | Open Access |
Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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U.S. DOE > Office of Science > Biological and Environmental Research (BER) | Advancing a Watershed Hydro-Biogeochemical Theory: Linking Water Travel Time and Reaction Rates Under Changing Climate | DOE:DEAC0205CH11231 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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