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Related Concept Videos

Typical Model Studies01:30

Typical Model Studies

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Fluid mechanics model studies often utilize scaled-down systems to predict fluid behavior in full-scale environments, such as river flows, dam spillways, and structures interacting with open surfaces. Maintaining Froude number similarity in river models is crucial, as it replicates surface flow features like wave patterns and velocities.
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Modeling and Similitude01:12

Modeling and Similitude

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Scaled modeling is a fundamental technique in engineering, enabling the study of large and complex systems by creating smaller, manageable replicas that recreate critical characteristics of the original. In hydrology and civil infrastructure, for example, scaled models of dams help analyze water flow, turbulence, and pressure. This method allows for accurate predictions of real-world behavior within a controlled environment, significantly reducing the cost and time involved in full-scale...
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A thermometer measures body temperature. The common sites for measuring body temperature are the oral cavity, axillary region, temporal artery, and skin surface, such as the forehead, abdomen, and axilla. True core body temperature is assessed in the rectum, tympanic membrane, pulmonary artery, esophagus, and urinary bladder.
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Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
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Related Experiment Video

Updated: Sep 18, 2025

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
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Identifying stream temperature variation by coupling meteorological, hydrological, and water temperature models.

Chunling Tang1, Valeria Garcia2

  • 1Office of Research, U.S. Environmental Protection Agency, Durham, North Carolina, USA.

Journal of the American Water Resources Association
|June 23, 2025
PubMed
Summary

This study coupled the River Basin Model (RBM) with VIC and WRF models to simulate Mississippi River Basin (MRB) water temperatures. Projections show significant warming, potentially impacting fish survival and exacerbating Gulf of Mexico dead zones.

Keywords:
RBM modelVIC modelWRF modelwater temperature

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Area of Science:

  • Environmental modeling
  • Hydrology
  • Climate science

Background:

  • Accurate water temperature modeling is crucial for understanding riverine ecosystems.
  • The Mississippi River Basin (MRB) faces potential impacts from climate change on its water resources.
  • Existing hydrological models require integration with water temperature modules for comprehensive analysis.

Purpose of the Study:

  • To develop and validate a coupled hydrological and water temperature model for the MRB.
  • To assess the sensitivity of MRB water temperatures to air temperature changes.
  • To project future stream temperature trends under climate change scenarios.

Main Methods:

  • Coupling the River Basin Model (RBM) with the Variable Infiltration Capacity (VIC) and Weather Research & Forecasting (WRF) models.
  • Physically based semi-Lagrangian approach for water temperature simulation.
  • Validation against observed water temperature data from six MRB river gages.

Main Results:

  • The coupled VIC-RBM model accurately simulates observed water temperatures in the MRB.
  • A 3.0°C uniform air temperature increase could raise MRB water temperatures by 1.3-1.8°C.
  • A 6.0°C air temperature increase could elevate water temperatures by 3.3-4.0°C.
  • Projected stream temperatures (2020-2099) show a 1.0-8.0°C increase, exceeding native fish survival thresholds in some areas.

Conclusions:

  • The coupled VIC-RBM model provides a robust tool for MRB water temperature assessment.
  • Projected warming poses significant risks to aquatic ecosystems and fisheries in the MRB.
  • Increased water temperatures will likely interact with nutrient loading, worsening harmful algal blooms and dead zones in the Gulf of Mexico.