Pt1420 Unit 6 Research

The process begins when the sun starts to heats up the surface which creates warm air. The warm, less heavy air rises and converges with the cold less heavy air above. This process is known as wind shears. Wind shears are when two

During June and July aerosol loading was comparatively higher at around 2-6 km height compared to the rest of the months. This possibly explains the high values of COF (figure 15 (b)) at higher altitudes in these two months due to convection processes that might have contributed to the formation of CCN (Jiang et al., 2007; Jiang et al., 2011). Excess rainfall events during 2013 ISMR, had resulted in heavy wash out of aerosols in the entire season which can be observed from low AOF values. The month of June witnessed an early onset of monsoon because of which there were more washouts of aerosols and September being the offset phase of the monsoon, witnessed high aerosol loading. July and August witnessed low AOF values, except that August had higher value of nearly 30% than that of June which had nearly 10-25% at 0.5-2 km altitude range The aerosol loading during June, July and August above the lower troposphere up to 4-6 km altitude might have contributed to cloud formation at higher altitudes which can be seen in the COF values of nearly 10-20%, 15-20% and 10-30% respectively at 12-17 km height range.

A molecular cloud is a giant condensation of dust and molecular gas. They are regions of relatively dense interstellar gas and dust with hydrogen molecules as well as carbon and silicate materials forming the primary constituents. Helium and small amounts of heavier elements are also found within the cloud. Molecular clouds are very cold and dark regions with typical temperatures of between 10 and 50 Kelvin. The mass of a typical

When I was reading Ona cloud rider I noticed that in one of the scenes they were good clouds and they were bad clouds, both sides different. So I went researching if they were different kinds of clouds. Yes they were different clouds, you can call them rain clouds or you can be more specific and call them high low or medium clouds. The groups are based on the height of the clouds kind of like some MLG tournaments how they referred some of their teams as A, D depending on what position they are in. My 2nd reason why this is real is look at some photographs at clouds, you can see tons of pictures about clouds and they are also some rarities of clouds like uncommon or rare clouds, an example

Is the process of forcing clouds to rain. Cloud Seeding involves flying a plane over clouds and dispensing silver iodide into the clouds. The silver iodide mimics ice crystals and gives the moisture in the clouds something to cling to, the moisture has clung to the silver iodide and is now snow this then is heavy enough to fall out of the clouds. The snow then melts into water then we have rain. Cloud Seeding is a very good solution to droughts because it is very area effective. It costs more than other solutions but for the area it covers it is efficient.

We know this can be induced because scientists have been experimenting with a practice called "cloud seeding" for decades.” Michelle Starr used this example of Logos to prove that increasing the amount of diesel exhaust fems increases cloud formation.

These clouds can exist undisturbed for extended periods, as they are quite able to withstand their own gravity, due to the low density and magnetic field that protects it from drifting into open space, and are considered to be stable. If a nearby, external

Have you ever seen a condensation trail from a plane (mainly jet) that persists in the sky? Unless you are extremely high in the atmosphere, that is not normal. They are actually chemical trails from dumping chemicals across the

In theory, the scientist Phil Plait says " the clouds coming from jets they are really just a product of condensation of water vapor. In newscientists.com, 77 scientists report that the results were surprising, 98.7% of scientists say that there is no atmosphere programing.

Nucleus - the central and most important part of an object, movement, or group, forming the basis for its activity and growth. When thinking about CDS, I have to think about the main person is at school and what immediately comes to mind is the head of school, Mr. Duncan. The reason I have chosen Mr. Duncan as the nucleus because he is the reason why we are expanding the school, he represents our school when he goes to conferences, talks more about how the school can improve.

First, tornados are formed by plenty of supercells. Actually, supercells are a huge cluster of thunderstorm clouds. In other words, heat rises up as it has a low vapor pressure and cold air drops down because of its high vapor pressure. (The National Severe Storms Laboratory) Because of this, the warm air in the end forms a vortex and forms a funnel cloud, also known as tornado.

The components that creates a thunderstorm includes moisture, instability and a lifting mechanism. These components are what determines the severity of a thunderstorm as well as an abundant of vertical wind shear. If the wind is weak in speed and direction, thunderstorms won’t reach hazardous weather.

Rain falls when clouds contain so much moisture that they can’t hold anymore and force it down to the ground. While all the moisture is still in the cloud, though, it acts as a sort of deflector for sunlight. Each individual drop of water that is in a cloud catch the sunlight, and therefore the solar radiation, and keep it from coming through to the earth. Clouds that are very bright have a lot of moisture in them that is catching the sunlight and deflecting it back.

When mountains, plains, and slopes have an upward breeze, it causes upslope fog. This fog can occur on the eastern side of the Rockies during the winter and spring (Ahrens, Samson 99).

The atmospheric parameters, including, aerosols, clouds, and precipitation, play very important role in our Earth’s climate system. The climate feedbacks influencing the global climate variability are directly or indirectly affected by aerosols, clouds, and precipitation, and thus, modulate the Earth’s radiation and surface energy balance. Therefore, global observations of aerosols, clouds, and precipitation are crucial not only to better understand the processes involved in the climate system but also to predict the future climate change.