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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.

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watershed-chemistry dissolved-organic-carbon nutrients metals high-mountain-watershed climate-warming

significant-stream-chemistry-response-to-temperature-variations-in-a-mountain-watershed's Introduction

Wei Zhi

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I am an assistant research professor in the Department of Civil & Environmental Engineering at Penn State University, University Park. My research interests focus on Critical Zone Science and Watershed Hydro-biogeochemistry. More specifically, I am interested in understanding how water moves and interacts with other components in natural environments. Ultimately, I aim to understand and forecast water quantity and quality at the watershed- and continental-scale, using both the process-based reactive transport model and the data-driven machine (deep) learning model.


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Research

Continential-scale water quality modelling & analysis

  • 2021, From Hydrometeorology to River Water Quality: Can a Deep Learning Model Predict Dissolved Oxygen at the Continental Scale?
  • 2020, The Shallow and Deep Hypothesis: Subsurface Vertical Chemical Contrasts Shape Nitrate Export Patterns from Different Land Uses

Watershed-scale hydro-biogeochemicy & reactive transport modelling

Wetland biogeochemistry, nitrogen transformation, and microbial community analysis

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