Clouds

When rain falls into a volcano, it can evaporate instantly due to the high temperatures of the volcanic surfaces. The water vapor may then mix with other volcanic gases and contribute to the volcanic activity, such as creating steam explosions or causing phreatic eruptions.

Cloud cover can be measured using satellite imagery, ground-based observations, and automated weather stations. Satellites can analyze the amount of light reflected by clouds to estimate their coverage. Ground-based methods involve visually estimating the percentage of the sky covered by clouds. Automated weather stations may use sensors to determine cloud cover based on the amount of sunlight reaching the surface.

The speed and direction of clouds are determined by wind patterns in the atmosphere. High-altitude winds, such as jet streams, can influence cloud movement, while vertical air currents can affect cloud speed. Additionally, factors like temperature, humidity, and air pressure can also play a role in cloud dynamics.

Tornadoes are made by thunderstorms, made by cumulonimbus clouds. They appear as very tall white puffy clouds with a dark base and an anvil shaped top. Thunderstorms that can produce tornadoes also have a corkscrew appearance or with striations in the cloud tower.

Three factors that must be present for cloud formation are;

hydroscopic nuclei, moisture, and cooling process.

Amounts of the above affect cloud formation.

Do you mean the affect of precipitation?

Or does this answer your question?

Furthermore, Precipitation will affect the mass of a cloud as well as evaporation and sublimation.

Hope this helps.

To get a fishing lure in Dark Cloud 2, you need to progress through the story until you reach the Starlight Temple. Inside the Starlight Temple, you can find a Lure Rod as a chest reward. This Lure Rod will come with a basic fishing lure that you can use to fish in various locations throughout the game.

There are two main types: stratus (flat layer) clouds and cumulus (tall bubbly) clouds.

As well as the two main types, high clouds are called Cirrus. Middle-level clouds are Alto. Rain clouds have Nimbus attached to them.

So:

Low-level clouds are

Stratus, Cumulus, Cumulonimbus and Stratocumulus.

Middle-level clouds are

Altostratus and Altocumulus

High-level clouds are:

Cirrus, Cirrostratus and Cirrocumulus.

A cloud that grows from low-level, through middle-level up to high-level, is called Nimbostratus and this deep cloud can bring heavy rain or snow that can last for several hours.

The original F or Fujita scale rates tornadoes from F0 to F5 based on the severity of damage and gives each tornado an estimated range of windspeeds based on this.

The EF or Enhanced Fuijta scale examines damage in more detail. Engineers and meteorologists look at the damage and determine the tornado's peak wind speed and use that to get the rating.

For example, if damage indicates a tornado had 120 mph winds at its strongest, it is rated EF2, with winds ranging from 111 to 135 mph

The wind estimates for the categories have been adjusted for the new scale, here is a comparison of the old and new. Keep in mind that even though the wind estimates for each category have changed the damage for those categories remains essentiall the same

F0 40-72 mph EF0 65-85 mph

F1 73-112 mph EF1 86-110 mph

F2 113-157 mph EF2 111-135 mph

F3 158-206 mph EF3 136-165 mph

F4 207-260 mph EF4 166-200 mph

F5 261-318 mph EF5 over 200 mph

When the fog will "burn away," it means that as the day progresses and the sun rises, the warm sunlight will cause the fog to dissipate and clear up, improving visibility. This typically occurs in the morning hours as the temperature rises and the atmosphere becomes less conducive to fog formation.

1 is used for measuring maximum and minimum temperatures

2 is used for measuring atmospheric temperature

3 is used for recording changes in air pressure

4 is used to see in which direction wind is blowing

5 is used for measuring wind speed

6 is used for measuring amount of rainfall

7 is used for measuring amount of humidity in atmosphere

A tornado is a violently rotating column of air that extends from a thunderstorm to the ground. It is capable of causing significant damage due to its high winds and can result in destruction of buildings and vegetation in its path. Tornadoes are commonly observed during severe thunderstorms.

In a surface low pressure system, air converges towards the center, causing a net inward movement. This convergence results in the air mass shrinking as it is forced to rise due to the lower pressure at the center of the system.

Antarctica. Maritime tropical air masses affecting North America typically originate from the Gulf of Mexico, the Caribbean Sea, or the western Atlantic Ocean.

Nimbostratus clouds typically give continuous rain due to their large, thick, and dark appearance. These clouds can cover the sky for long durations and produce steady precipitation.

Particles of matter absorb energy during melting and vaporization processes, as these transitions involve the breaking of intermolecular forces that hold the particles together. During freezing and condensation processes, particles release energy as they form stronger bonds and lower their energy levels to create a more stable state.

A cold front is formed.

Yes a cold front is formed, but this could also come to mean that a cold front overtakes a warm front which means a new front would be formed called an occluded front.

Mist is a common sign of fog and is very light

Fog is very thick and sometimes we can not see at all

Mist ussally means low clouds

Fog does mean very low clouds with some kind of water it ussually takes place in winter

When water evaporates, it is generally quite pure, but while suspended in the atmosphere, it is exposed to dust particles that become part of the condensate, so the resulting water is not pure, but contaminated with the solid particles that are in the atmosphere in the same vicinity.

tall and dense, puffy, bunny tail like

Fast-moving clouds are typically a sign of strong winds in the upper atmosphere. This could indicate an approaching weather system or a change in weather conditions. Rapid cloud movement may also lead to quick changes in visibility and sudden weather changes.

In a high-pressure system, air rotates in a clockwise direction in the northern hemisphere and counterclockwise in the southern hemisphere. In a low-pressure system, air rotates counterclockwise in the northern hemisphere and clockwise in the southern hemisphere. This is due to the Coriolis effect caused by the Earth's rotation.

An air mass's stability refers to its ability to resist vertical movement- more stable air resists rising and sinking motion. Stable air masses typically have cooler, denser air near the surface, preventing strong vertical movement. Conversely, unstable air masses are more prone to rising due to warm, buoyant air near the surface.

Rains associated with cold fronts tend to be shorter in duration but more intense, while rains from warm fronts are typically longer-lasting but less intense. Cold fronts move faster and have steeper slopes, leading to quick, intense rainfall followed by clearing skies. Warm fronts have more gradual slopes, resulting in longer periods of lighter rainfall.

This can be either sleet or freezing rain, though both technically start as snow and melt into rain. Sleet is rain that is able to freeze back into ice pellets before reaching the ground. Freezing rain is rain that does not have enough time to freeze into ice before reaching the ground - the cold layer is very shallow to the ground, so it is rain that freezes on contact with cold surfaces.

This is usually adiabatic cooling. Adiabatic refers to a process that does not exchange heat with the air around it. Air that is adiabatically cooled is cooled only because the decreasing pressure with height forces it to cool.