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Related Concept Videos

Temperature Measurement Sites01:14

Temperature Measurement Sites

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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.
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
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Precipitation Gravimetry01:03

Precipitation Gravimetry

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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.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
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Precipitation Processes01:12

Precipitation Processes

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The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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Types of Coprecipitation01:10

Types of Coprecipitation

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Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
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Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

1.7K
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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Coordinates and Map Projections01:29

Coordinates and Map Projections

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Coordinates and map projections are essential tools in accurately representing the Earth's surface for various applications, ranging from navigation to spatial analysis. The latitude and longitude coordinate system is a universally recognized framework for defining locations. Latitude specifies the distance of a point north or south of the equator, measured in degrees from 0° at the equator to 90° at the poles. Longitude indicates a location's position east or west of the prime meridian,...
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Bias-corrected high-resolution temperature and precipitation projections for Canada.

Hebatallah M Abdelmoaty1,2, Chandra Rupa Rajulapati3, Sofia D Nerantzaki4

  • 1Department of Civil Engineering, Schulich School of Engineering, University of Calgary, Calgary, Canada.

Scientific Data
|February 1, 2025
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Summary

A new database provides high-resolution climate projections for Canada until 2100. This resource uses Semi-Parametric Quantile Mapping (SPQM) to bias-correct climate model data for better risk assessment and planning.

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Area of Science:

  • Climate Science
  • Environmental Science
  • Data Science

Background:

  • High-resolution climate projections are crucial for effective decision-making, risk assessment, and planning in Canada.
  • Existing climate model data often requires bias correction to accurately represent observed conditions.

Purpose of the Study:

  • To develop an extensive database of high-resolution (0.1°) daily precipitation and temperature projections for Canada until 2100.
  • To bias-correct Coupled Model Intercomparison Project, Phase-6 (CMIP6) climate model outputs using a novel methodology.

Main Methods:

  • Developed and applied the Semi-Parametric Quantile Mapping (SPQM) methodology for bias correction.
  • Utilized four Shared Socio-economic Pathways (SSPs) to analyze future climate scenarios.
  • Compiled a comprehensive database (SPQM-CMIP6-CAN) encompassing numerous climate model simulations.

Main Results:

  • The SPQM methodology effectively reproduces observed marginal properties, trends, and variability.
  • The database includes 693 precipitation simulations from 34 climate models and 581 temperature simulations from 27 climate models.
  • Projections extend daily to the year 2100 at a 0.1° resolution for Canada.

Conclusions:

  • The SPQM-CMIP6-CAN database offers a valuable, high-resolution resource for hydrological, environmental, and ecological studies in Canada.
  • This database aids in quantifying uncertainties associated with different climate models, configurations, and future scenarios.
  • The findings support improved climate change adaptation and mitigation strategies through enhanced data accessibility and reliability.