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What does a cloud mirror measure?

Published in Cloud Cover Measurement 2 mins read

A cloud mirror, or more accurately, using a mirror to assess cloud cover, measures the area of the sky covered by clouds.

Understanding Cloud Cover Measurement

Cloud cover is a fundamental aspect of meteorology and climatology. It plays a crucial role in weather forecasting and climate modeling. While a simple mirror can aid in this process, it's important to understand the nuances of cloud cover measurements:

  • Visual Estimation: Mirrors are used to aid in the visual estimation of cloud cover. By reflecting the sky, a mirror makes it easier to assess how much of the sky is obscured by clouds.
  • Oktas: Traditionally, cloud cover is often measured in oktas, where the sky is divided into eight parts. Each okta represents one-eighth of the sky covered by clouds. For example, 0 oktas mean a clear sky, and 8 oktas mean a completely overcast sky.
  • Limitations: According to the provided reference, it is important to note that while a mirror may facilitate a visual assessment of cloud cover, "oktas only estimate cloud cover in terms of the area of the sky covered by clouds." This measurement method does not account for:
    • Cloud Type: The kind of clouds present (e.g., cirrus, cumulus, stratus).
    • Cloud Thickness: How dense or opaque the clouds are.

Practical Implications

These limitations are important to consider because cloud type and thickness significantly affect factors like:

  • Albedo: The amount of solar radiation reflected by clouds back into space. Thicker clouds with a higher albedo will reflect more sunlight.
  • Surface Solar Radiation: The amount of solar energy that reaches the Earth's surface. Thicker and more extensive cloud cover will reduce the amount of solar energy reaching the surface.

Conclusion

In summary, a cloud mirror, when used as a tool for visual estimation, primarily measures the area of the sky covered by clouds, and not other crucial factors like cloud type or thickness. Therefore, it is important to consider these limitations while using such measurements for estimating cloud albedo or surface solar radiation.

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