Description Of A Virtual Meteorological

Even if you cannot tell the difference between the cultures of Hawaii and Florida, the weather easily sets the two apart. As far as tropical locations go, many people expect the weather to be warm and sunny, looking for a perfect day to go to the beach and relax next to the ocean. In Florida, though the heat and humidity is almost unbearable. It makes you want to immediately jump into the ocean to try a cool off under the hot sun. Unfortunately, with the sun beating down on the ocean and the humidity in the air trapping all of the heat, the ocean also heats up very quickly and it becomes more like a hot tub, which is not the most relaxing of choice in the middle of a warm, summer day. With all of the humidity in Florida, it is also very common for a sudden downpour to erupt and leave you soaking wet like you have been in the ocean all day. Despite these flaws in the perfect, tropical weather you expect, when you do get a nice day in Florida, it makes you wish the day would never end and that you would never have to leave.

suspected it consisted of a single curved line and a single straight one. For my retests, I studied it

the composite or generally prevailing weather conditions of a region, as temperature, air pressure, humidity, precipitation, sunshine, cloudiness, and winds, throughout the year, averaged over a series of years.

Frost forms when there is enough moisture in the air and the ground is cold to

Climate is an atmospheric change in the average weather in an area over a period of

So the warm moist air creates clouds of rain and thunderstorm. Adding to that winds with different speed going in different directions assisting in expanding these great clouds of rain and thunderstorm. With

Roger A. Pielke Jr. and Roger A. Pielke Sr. in their book Hurricanes: Their Nature and Impacts on Society, state that the hurricane is a member of a phenomena called cyclones, which refers to “any weather system that circulates in a counterclockwise direction in the Northern Hemisphere and in a clockwise direction in the Southern Hemisphere” (p.15). The word

The picture to the left is an example of using lines to lead the viewers eye. The actual line in the center of the page directs the eye up the picture to the mountains. The

This causes the global variance in temperature to decrease, which in turn has an effect on the weather pattern in many places. In meteorology, a jet stream is formed when cold air meets with hot air. This fast flowing, and narrow stream of air helps push out the current weather conditions and assists with the changing of seasons. Since the strength of jet streams rely on the variance between the different air masses, having a warming Artic will only weaken the strength of jet

Warm air rises and cool air sinks, or subsides. If the Earth had no continents and did not turn, then the circulation of the atmosphere would appear much like this.

An air mass is a large body of air in Earth’s lower atmosphere, and it contains similar characteristics throughout. For example, in an air mass, the temperature is almost the same. The temperature of an air mass depends on where it originates. As air masses travel, their characteristics may change. As cold air from the poles moves south, the air temperature slowly heats up as a result of moving over a warmer surface. Because two opposing air masses do not easily mix, they have an area that separates them, called a front. The size of a front can vary greatly. The width of a front can be anywhere from 200 meters to 200 kilometers. They can be as high as five kilometers, and they can even reach 2000 km in their length (about as long as the north-south distance of the continental United States!) Fronts occur most often at mid-latitudes because that is where tropical air moving north, and southward moving polar air often meet. Because

There are five different primitive equations that are being used to predict the weather, Wind forecast equation, it is the equation of motion that explains the movement of air masses in the atmosphere, the continuity equation deals with the rising of warm, wet air and sinking of cold dry air as the air columns shrinks and stretches, and then according to Tyson & Preston-Whyte(2000:342) the temperature forecast equation helps the climatologists and meteorologists to see that, there is local changes in temperature because of the horizontal advection of temperature and there is also changes in distribution of heat when the adiabatic latent-heat is added to the earth surface and the atmosphere, moisture forecast equation shows that when condensation, precipitation and evaporation occurs,

Climate happens between earths atmosphere and ocean.This is where energy is exchanged This is where great amount of water evaporate into the air or fall back as rain warm air around the equator rises and goes north towards the pole in the northern hemisphere.​we live at the bottom of an ocean of air. Air is made of nitrogen.oxygen, carbon dioxide,water vapor and many other different molecules and atoms on a gaseous state.Air pressure is the force per unit area applied on a surface by the weight of the air above the surface .altitude affects air pressure.Air pressure changes when the air itself is heated or cooled.Wind is the horizontal movement of air from a high pressure area to a low pressure area.To understand the effects of winds on

episode. Normally, during the day the air near the surface is heated and as it

When we went back to school this quarter, I was looking forward to learning about blueprints. I have worked with AutoCAD before, but I didn’t know something as simple as the meaning of the lines in a set of