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Boundary Layer Characteristics01:18

Boundary Layer Characteristics

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When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
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Precipitation Processes01:12

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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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Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

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During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
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What is Climate?01:16

What is Climate?

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Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
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States of Water01:23

States of Water

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Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
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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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Related Experiment Video

Updated: May 5, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
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The missing mountain water: slower westerlies decrease orographic enhancement in the Pacific Northwest USA.

C H Luce1, J T Abatzoglou, Z A Holden

  • 1U.S. Forest Service Research and Development, 322 East Front Street, Boise, ID 83702, USA.

Science (New York, N.Y.)
|December 3, 2013
PubMed
Summary
This summary is machine-generated.

Declining winter westerlies reduced mountain precipitation and streamflow in the Pacific Northwest. This study reveals differential precipitation trends across elevations, impacting hydrology under climate change.

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Area of Science:

  • Hydrology
  • Climatology
  • Meteorology

Background:

  • Streamflow declines in the Pacific Northwest were previously attributed to rising temperatures.
  • Precipitation trends at lower elevations were found to be negligible, suggesting other factors at play.

Purpose of the Study:

  • To investigate the role of differential precipitation trends across elevations in explaining observed streamflow declines.
  • To identify the atmospheric drivers of these precipitation trends.

Main Methods:

  • Analysis of historical precipitation data across different elevations in the Pacific Northwest.
  • Correlation analysis between winter westerly wind patterns and precipitation at high and low elevations.
  • Examination of climate model projections for future atmospheric circulation and precipitation.

Main Results:

  • Observed streamflow declines are linked to reduced precipitation, particularly at higher elevations.
  • Winter westerly winds (November to March) show a strong correlation with high-elevation precipitation but a weak correlation with low-elevation precipitation.
  • A significant decrease in lower-troposphere winter westerlies from 1950 to 2012 is associated with reduced orographic precipitation enhancement.

Conclusions:

  • Declines in winter westerly winds have led to differential precipitation trends across elevations, contributing to reduced streamflow.
  • Weakened atmospheric zonal flow under future climate change scenarios poses an additional threat to Pacific Northwest hydrology.