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When spring finally arrives in the mountains, the snow pack may be two meters deep, composed 50%of ice and 50%of air. Direct sunlight provides about 1000watts/m2to earth's surface, but the snow might reflect 90%of this energy. Estimate how many weeks the snow pack should last, if direct solar radiation is the only source of energy.

Short Answer

Expert verified

t=733300s=35.5daysthe anow pack last.

Step by step solution

01

Step :1 Snow composed

Suppose the snow is composed of 50%ice and 50%air, and that it's 2metres deep. The sun provides around 1000watts of power, but around localid="1650328444025" 90%of this is reflected by the snow, so the snow absorbs only about 100 watts.

02

Step : 2 Density of melting point 

The density of ice melting point is

ρ=0.9167gcm3=0.9167gcm3×106cm3m3

ρ=9.167×105gm3

Because snow is made up of 50% ice and 50% air, there is a mass mof ice in a block of snow with a surface area of 1m2and a depth of 2m:

m=50100ρ×V=129.167×105g×(2×1)=9.167×105g

To melt the ice, you'll need the following quantity of heat:

Q=m×L

where Lis the latent heat, and its for melting ice, so:

Q=9.167×105×80=7.333×107cal

but 1cal=4.184Jis,

Q=4.184×7.333×107cal=3.068×108J

03

Step : 3 Sun generates heat

The sun generates heat in the form of:

P=QtA

where tis the amount of time that the region Amust be exposed to the heat Q, the time is:

t=QPA

Substitute Q=100watts,A=1m2andQ=3.068×108cal, so:

t=3.068×108100×1

role="math" localid="1650328384083" =3068000s

t=733300s=35.5days

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Most popular questions from this chapter

In Problem 1.16 you calculated the pressure of the earth’s atmosphere as a function of altitude, assuming constant temperature. Ordinarily, however, the temperature of the bottommost 10-15 km of the atmosphere (called the troposphere) decreases with increasing altitude, due to heating from the ground (which is warmed by sunlight). If the temperature gradient |dT/dz|exceeds a certain critical value, convection will occur: Warm, low-density air will rise, while cool, high-density air sinks. The decrease of pressure with altitude causes a rising air mass to expand adiabatically and thus to cool. The condition for convection to occur is that the rising air mass must remain warmer than the surrounding air despite this adiabatic cooling.

a. Show that when an ideal gas expands adiabatically, the temperature and pressure are related by the differential equation

dTdP=2f+2TP

b. Assume that dT/dzis just at the critical value for convection to begin so that the vertical forces on a convecting air mass are always approximately in balance. Use the result of Problem 1.16(b) to find a formula for dT/dzin this case. The result should be a constant, independent of temperature and pressure, which evaluates to approximately 10°C/km. This fundamental meteorological quantity is known as the dry adiabatic lapse rate.

Make a rough estimate of how far food coloring (or sugar) will diffuse through water in one minute.

Given an example to illustrate why you cannot accurately judge the temperature of an object by how hot or cold it feels to the touch?

Calculate the total thermal energy in a liter of helium at room temperature and atmospheric pressure. Then repeat the calculation for a liter of air.


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