Absorption Fraction Feedback Plotss For The Study Area

The soil loss water due to evapotranspiration process and the water level will be recharged through precipitation. In the tropical rainforest, precipitation rate are high due to high evapotranspiration rate. High evapotranspiration rate plays a significant role in cloud formation above the rainforest area and its surroundings. Water vapour that is released into the air will be condensed as it moves to a higher altitude. The condensed water vapour form the clouds above the forest. The more water vapour being released into the air, the more clouds would be formed.

From the CER maps (Figure 9), it can be observed that in 2013 ISMR the entire region had witnessed high CER values while other years were partially cover by cloud drops of different radii. The high rainfall intensity during 2013 ISMR could be the manifestation of the high CER values observed during that year compared to the other years (Figure 12). However, the low CER values in the other years can be seen in conjugation with high aerosol loading during that period. Similar trend is also observed in LWP plots for the study area during 2012-15 ISMR (Fig 13). It is evident from the figure 9 that LWP varies from low to high values over the region while, it is more homogeneous in 2014 and 2015 ISMR. The OLR was considerably

The Rain Shadow Effect also plays a major role in climate formation. Clink on the link below to learn about the Rain Shadow Effect. Be sure to read the Introduction. Then, click on the Animation and choose “narrated” at the bottom. Then, read the conclusion and see how you do on the practice quiz. Once you have done that, answer the questions below.

Clouds to form in the atmosphere have to have water vapor present. This water vapor makes up a cloud. The water vapor in the atmosphere comes from evaporation or deposition. Also the temperature of the air is below the dew point. When the water is fully saturated, it starts to rise and the expansional cooling process begins. During the process of condensation, the aerosol particles act like a nuclei in the atmosphere, which began to grow, creating ice crystals that are big enough to produce a cloud.

Quito is the capital city from Ecuador where is considering a high elevation area with approximately 2800 meters above sea level in its elevation. Also, the city is located in the center of Andean Region and it is influenced by the equatorial line with latitudes nearest to 0 grades and being in a Tropical Region without seasons (Figure 1). Moreover, Quito doesn’t present stations, only the city shows two times considered like a dry and a wet season. The mean temperature during the year has a mean in minimum about 9.0°C and a maximum 25.4 °C20, also presented a high precipitation near to 1126 mm on 2015 that let to have a high density cloud every year.

GEOG 104 – Weather Climate Society: You have gotten 283.5/425 66.7% of the available points thus far. I know that this is your most difficult class; however, I have seen you working with your assigned tutor for this class. Please, come every day to prepare for this class. Your Exam # 2 is going to be given this Thursday, November 12th, contact your tutor and prepare very well for this

St. Louis falls into the mellow midlatitude atmosphere gathering, and this is a district loaded with air mass complexities (Hess, 2011). These differentiations cause a mixture of unsettling influences in the air leaving St. Louis with an assortment of climate (Hess, 2011). The summers have a tendency to have more precipitation with the coastal stream and incessant convection (Hess, 2011). However winter can encounter rain and periodic snow due to midlatitude typhoons (Hess, 2011).

Brimblecombe, P. (1981). Long term trends in London fog. The Science of The Total Environment Online, 22(1), 19-29. doi:10.1016/0048-9697(81)90078-4

Weather is created by the movement of air masses of different temperature and moisture content moving around the Earth’s atmosphere and interacting with each other.

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

Cloud seeding is when a cloud gets seeded with chemicals to produce more rain. For a cloud to produce rain the temperature in the cloud needs to be below the freezing point of water. When reached below the freezing point the cooled water has meet specks of dust,

Our climate is forever changing. Thus causing our planet to heat up. Some parts of the earth are receiving less than average precipitation than is needed, this is causing droughts. Cloud seeding is the best solution to mitigate the effects of droughts. Although cloud seeding is more expensive than other alternatives, it is more area efficient and the most effective way to mitigate the effects of a drought. This report will give you a full insight about a drought and how to mitigate it’s effects.

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.

This continual warming of air actually allows for even more water vapor to be stored, and it is this feedback loop that is cited as the principle reason water vapor is considered to be the most effective greenhouse gas. Although he stresses that water vapor accounts for a substantial amount of climate change, Emanuel does not neglect to mention the involvement of industrial activity, biomass burning, and sulfate aerosols. The concept of “climate noise” is introduced within the final two pages of chapter three, but the author may have fortified the argument for global warming by spending a few more pages on the compelling concept, perhaps devoting an entire chapter to it.

I was never very familiar with the term May Gray or June Gloom until I moved to California. I grew up on the Oregon coast and it is weird to me that I never knew those terms existed! I remember the first time that I heard the term June Gloom, I was thinking, what the heck is that? I was in San Diego at the time and I actually asked what the term meant but the local didn’t describe it clearly so of coursed I looked it up. This article was interesting and it went in depth to what these terms meant and how these low clouds are formed. Also I thought it was fascinating that researchers can also predict the marine layer clouds a head of time!