An example of the effect of wind
convection currents
The lumpy white clouds are called, Cumulus. Cumulus clouds are found in the lower section of the sky. They are often described as puffy or lumpy, they generally have flat bases. Cumulus clouds are generally less than 6,500 ft. Cumulus clouds may appear by themselves in a line or in clusters.
Clouds are all different shapes and sizes. Now, this is because of the water vapour. It doesn't settle in a straight line, partly because it doesn't want to! There are no two clouds in the sky that are the same. It is similar with zebras, There are no two zebras with the same stripes.
Rainbow forms by lots of tiny particles in the air. So this is how it works: After it has rained, the thunder makes sound down to earth. It goes into the clouds, and when the clouds trim away, it leaves gas which form a trail of fog. It also leaves behind the particles formed inside the clouds, just like as if you rub paint against paper. After, the tiny particles go into other type of clouds, called cirruculum clouds. The clouds have gas colours of red, orange, yellow, green, blue, indigo, and violet. The particles gets stained by one color, and end at the horizon line to stop moving. That is also called evaporating. They stop at a circumstansed movement line, so they line up against each other. That is how rainbows form colour.
467866878
An example of the effect of wind
An example of the effect of wind
An example of the effect of wind
An example of the effect of wind
An example of the effect of wind
An example of the effect of wind
An example of the effect of wind
convection currents
convection current
convection currents
Reflection
the slope tells you the angle to draw a line. for example the slope 3/5 tells you that line line rises 3 units for every 5 units it moves across the x axis. this can be remembered by rise over run.