Moisture Content: The amount of water vapor present in the atmosphere influences the formation and persistence of clouds. Higher moisture levels can lead to increased cloud cover.
Atmospheric Stability: The stability of the atmosphere determines the vertical movement of air and can impact the development of clouds. Unstable air may lead to more cloud formation.
Topography:Landforms can affect local air currents and cloud formation. Mountain ranges, for example, can cause orographic lift, resulting in increased cloud cover on the windward side.
Types of Cloud Cover
Cloud cover is often classified based on the fraction of the sky obscured by clouds. Common categories include:
Clear Sky (0/8): When no clouds are present, the sky is considered to have 0/8 cloud cover.
Partly Cloudy (1/8 - 5/8): This refers to a sky with some cloud cover, but with significant portions remaining clear.
Mostly Cloudy (6/8 - 7/8): A sky with a high percentage of cloud cover, but with some clear patches.
Overcast (8/8): When the entire sky is covered by clouds, the cloud cover is considered to be 8/8.
Measuring Cloud Cover
Cloud cover is typically measured using instruments such as ceilometers, satellites, and weather radar. Additionally, it can be visually estimated by trained observers using standardized methods. One common technique is the Okta scale, which quantifies cloud cover in eighths, with 0 indicating clear skies and 8 representing completely overcast conditions.
Create a computational model to calculate the change in the energy of one component in a system when the change in energy of the other component(s) and energy flows in and out of the system are known.
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.