Penney Corporation, respectively, you will calculate and compare the financial ratios listed further down this documentfor the fiscal year ending and prepare your comments about the liquidity, solvency and profitability of the two companies based on your ratio calculations. The entire project will be graded by the instructor at the end of the final submission in week 7 and one grade will be assigned for the entire project. Overall Requirements For the Final Submission:
March 26, at 3: Throughout the internet, you can see a lot of comments about the long "chemtrails" of climate engineering and about the short "condensation trails" that are not the same thing as the longer trails that remain in the air after the spraying. But is it true that the "short trails of condensation" sometimes with 50,or times the length of the airplanes are not also trails of aerosols?
These shorter trails of aerosols are seen in much higher altitudes, in the stratosphere, and the density of the stratosphere is very different than the atmospheric density of the troposphere. And it is because of this fact that the trails of aerosols do not stay a long time under the form of a long line and start dissipating very fast in a very thin stratosphere where the horizontal circulation of gases and particles occurs very quickly: The lowest layer is the troposphere, which extends from the surface to the bottom of the stratosphere.
Three quarters of the atmosphere's mass resides within the troposphere, and is the layer within which the Earth's terrestrial weather develops.
The depth of this layer varies between 17 km at the equator to 7 km at the poles. The stratosphere, extending from the top of the troposphere to the bottom of the mesosphere, contains the ozone layer. The ozone layer ranges in altitude between 15 and 35 km, and is where most of the ultraviolet radiation from the Sun is absorbed.
The top of the mesosphere, ranges from 50 to 85 km, and is the layer wherein most meteors burn up. The thermosphere extends from 85 km to the base of the exosphere at km and contains the ionosphere, a region where the atmosphere is ionised by incoming solar radiation.
The ionosphere increases in thickness and moves closer to the Earth during daylight and rises at night allowing certain frequencies of radio communication a greater range. The exosphere begins variously from about to 1, km above the surface, where it interacts with the planet's magnetosphere.
Each of the layers has a different lapse rate, defining the rate of change in temperature with height. The lowest part of the troposphere, where friction with the Earth's surface influences air flow, is the planetary boundary layer.
This layer is typically a few hundred meters to 2 km 1. Atop the troposphere is the tropopause, which is the border between the troposphere and stratosphere. The tropopause is an inversion layer, where the air temperature ceases to decrease with height and remains constant through its thickness.
Most of the phenomena associated with day-to-day weather occur in the troposphere. Air also contains a variable amount of water vapor. Except for the water vapor content, the composition of the troposphere is essentially uniform. The source of water vapor is at the Earth's surface through the process of evaporation.
The temperature of the troposphere decreases with altitude. And, saturation vapor pressure decreases strongly as temperature drops.
Hence, the amount of water vapor that can exist in the atmosphere decreases strongly with altitude and the proportion of water vapor is normally greatest near the surface of the Earth. The stratosphere is stratified in temperature, with warmer layers higher and cooler layers closer to the Earth.
The increase of temperature with altitude is a result of the absorption of the Sun's ultraviolet radiation by the ozone layer.
This is in contrast to the troposphere, near the Earth's surface, where temperature decreases with altitude. The border between the troposphere and stratosphere, the tropopause, marks where this temperature inversion begins.
Near the equator, the stratosphere starts at 18 km 59, ft; 11 mi ; at mid latitudes, it starts at 10—13 km 33,—43, ft; 6. Temperatures vary within the stratosphere with the seasons, in particular with the polar night winter.Course Project 2 Assignment Comparing Kohl's and leslutinsduphoenix.com Essay Words | 4 Pages (% - %) Net Sales $18, $17, Profit margin ratio Net Income $1, = % $ = % Kohl's is more profitable based on the profit margin ratio because it earns 6 cents for every $ in sales as compared to 2 cents earning per $ of JC Penney.
Course Project 2 Assignment Comparing Kohl's and leslutinsduphoenix.com Essays tremendously. Current ratio Current assets $5, = $6, = Kohl's inventory turnover is slightly better by.3 . COURSe PROJECT The following is the information needed for the course project: 1-Project Material: Students are required to obtain an annual report and K form of two publicly held companies (other than the two companies used for final exam) for two consecutive years to be used for the project.
2- Project Learning Objectives:The primary. Your Course Project Financial Statement Analysis Project—A Comparative Analysis of Oracle Corporation and Microsoft Corporation. Here is the link for the financial statements for Oracle Corporation for the fiscal year ending /5(1). Course Project 2 Assignment Comparing Kohl's and leslutinsduphoenix.com Essay Words | 4 Pages Khol's Corporation JC Penny Corporation Earnings per share As given in the income statement $ $ The comparison of these two numbers are not meaningful, the number of .
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