Identify And Explain The Factors That Cause Changes In Long Form

As storm relative velocity helps analyze the motion of the winds within the storm, information like the rotation of the storm and the speed of the winds can help investigate the chances of the storm developing into a tornado. If the storm appears to be a threat, nearby communities can be notified to take precautions and leave if necessary. Although base velocity can be used for the same reason, the speed of the storm can affect the results of the speed and rotation of winds. Therefore, storm relative velocity is more accurate and reliable than base velocity in determining the threat of a

If you look at storm 2 and storm 3’s temperatures before the storm, it’s a drastic difference. Storm 2 was 81 degrees fahrenheit and storm 3 was 104 degrees fahrenheit. Storm 2 had only 5 inches of rain, while storm 3 had 8 inches of rain. Based on temperature being one of the only variables, I concluded that warmer weather caused Galetown to have more severe storms.

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.

Not only did weather affect the plot, but huge natural disasters also affects the plot. On page 81, it says, “I looked and saw the entire portable being swallowed up by the mud, it’s roof now where it’s porch steps

Growing up, we all went through the water cycle lesson and we will never forget it. The reason being, we encounter the water cycle throughout our entire life and it will always effect our systems and more importantly our water system. As illustrated in the picture, our water cycle includes the processes of evaporation, condensation, precipitation, which then goes to many places. During evaporation, the sun is used as a main power to make this happen. The sun’s rays beat down onto the ground creating all of the moisture and water to fizzle into a gas state into the atmosphere and get stored away into the clouds. When it is stored into the clouds it is condensing. Condensation means that the gas is again forming itself back into its liquid state to get ready to return to Earth. The condensation then forms into precipitation. Precipitation comes in many different forms. You can see it as rain, snow, sleet, or hail making its way back to us. What happens to it then depends on the area. The water might end up as runoff, or become

As with the huge snowstorm of December 1974 another even more powerful (in terms of intensity/extent) storm is of strong interest to all meteorologists who have studied winter storms in the Great Lakes. This storm is also of interest and remembrance to many longtime residents of the Great Lakes, the Upper Ohio Valley and Ontario, Canada who had to deal with winter's full fury late in January of 1978. In addition, the storm certainly casts many memories for those of us who were on duty and worked during the storm...while being in awe of the development and subsequent immense strength of this great monster. With the 30th anniversary of this Great Blizzard at hand, it is worth taking a step back in time to re-live this monumental example of nature's fury.

There is speculation that climate change may have also have contributed to the storms intensity. Global warming may have made Sandy wetter and stronger. Hurricanes and tropical storms are fueled by warm water evaporating into the air. Records indicate that ocean surface temperatures are up 0.9 degrees

In this document, I jotted down some notes while putting together the reading material. These notes point out some of the reading content to pay particular attention to. The notes are divided into section headings based on the reading material. This is not meant to be a complete list of everything that you need to know from the reading Water in Atmosphere You should know what is meant by phases of water and phase changes of water. Water vapor is extremely important in the atmosphere for many reasons. A few of those reasons include Water vapor transforms into both liquid and solid cloud particles that grow and fall to Earth as precipitation. When water vapor condenses in the formation of clouds, large amounts of heat - calledlatent heatis

“Weather is just weather. It’s never just rain” (44). If a setting in a story involves rain it’s not because outside was hot and all the water evaporated into the clouds and couldn’t hold anymore so it started to pour. I mean who would ever think of such a thing? Usually when a story contains raining it can mean the character is being “purified” or transformed. However with rain comes mud, which can cause the character to be more tainted then before. Rain is also associated with spring, which is a period of rebuilding and all the more imperatively, trust. Mist can include the wretchedness element, additionally disarray among characters and circumstances. Snow is generally as critical and negating as downpour. It can be spotless, welcoming, lively, or even warm (like a protecting blanket).However it can likewise be stark, serious, cold choking, and even grimy. The Great Gatsby, by F. Scott Fitzgerald, Gatsby and Daisy's get-together starts amidst a deluge which

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

Increased frequency and intensity of storms and weather extremes may increase safety and health risks for vulnerable populations including water ingress, mould and loss of housing for poorly housed and health risk to the homeless.

Weather is the state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity, and barometric pressure. Weather can be classified as day to day temperature and precipitation activity, where climiate is average atmospheric conditions over longer periods of time. Weather occurs from temperature and moisture differences between one place and another. These differences can occur due to the sun angle at any particular spot. The strong temperature contrast between polar and tropical air gives rise to the jet stream. Weather systems in the mid-latitudes, such as "extratropical cyclones", are caused by instabilities of the jet stream flow. Because the Earth's axis is tilted

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).

The ability help to develop the thunderstorms. The tornadoes happen more frequent in the noon and evening, right next to the heat of the day that has made the hot air that starts thunderstorm and remember a thunderstorm leads to a tornado. Thunderstorm can happen when moist and warm air gets stuck by warm, dry air below a layer of cool dry air this is call an inversion.Most tornadoes come from thunderstorms. Warm moist air from the Gulf of Mexico and dry cool air from Canada. When these two air masses meet they create instability in the atmosphere. A change in wind direction and speed. Along with increasing height the air spins 2-6 miles wide and cause a tornado. A natural disaster if you will most of the moist will start things up, some of the key ingredients putting into an unstable atmosphere is warm and moist air at low

c. “It is well known that tropical cyclones form only over warm oceans from which they gain their energy, largely from the latent heat of condensation. Thus, it would not be surprising if a warmer and moister world contained enhanced overall hurricane activity” (Anthes, R. et al., 2012, 624).