Concept explainers
If the insolation of the Sun shining on seawater is 8.7
The change in temperature of a
Answer to Problem 13PEB
Solution:
Explanation of Solution
Given data:
Insolation of the sun is
The albedo of the sea water is
The area of the layer at the surface
Time is 1 hr.
Density of seawater is
Thickness of the layer of seawater is
Specific heat of seawater is
Formula used:
Write the equation for the incoming solar radiation by the reflected solar radiation to determine the albedo.
Here,
Write the equation for energy from the absorbed solar radiation:
Here,
Write the formula for density.
Here,
Write the formula for volume:
Here,
Write the formula for heat:
Here,
Explanation:
Determine reflected radiation:
Recall the equation for the incoming solar radiation by the reflected solar radiation to determine the albedo, denoted by alpha.
Substitute
Convert hours to seconds:
Determine energy:
Recall the equation for energy from the absorbed solar radiation:
Substitute
Determine the mass of seawater:
Convert
Recall the formula for volume.
Recall the formula for density.
Substitute
Substitute
Convert energy to calorie heat:
Determine the temperature change of seawater.
Recall the formula for heat:
Substitute
Conclusion:
The change in temperature is
Want to see more full solutions like this?
Chapter 22 Solutions
Physical Science
Additional Science Textbook Solutions
Physical Universe
Physics for Scientists and Engineers: A Strategic Approach, Vol. 1 (Chs 1-21) (4th Edition)
Physics: Principles with Applications
Introduction to Electrodynamics
College Physics: A Strategic Approach (4th Edition)
The Physical Universe
- The following data are given for the pressure and temperature variation in air as a function of elevation: Elevation in [m] 0. Temperature in [°C]_pressure [atm] 28 1. 1000. 25 0.796 2000. 19 0.6314 3000. 12 0.4982 4000. 3 0.3905 5000. -1 0.3043 6000. 11 0.2356 You want to check if these measurements are correct. You are going to use a balloon and rise in the corresponding altitudes. If the balloon weighs 1000kg (all included, weight of yourself, equipment, inflated part etc) calculate the volume of inflated part of the balloon, so that the initial acceleration is 15m/s?. Assume that the balloon is a sphere and neglect the deflated part of the balloon as far as volume is concerned. Can you verify all measurements with this volume of the balloon? What kind of adjustments do you need to make in order to complete your mission?arrow_forwardA body radiates heat at the rate of 5 cal/m² s when its temperature is 227°C. The heat radiated by the same body when its temperature is 727°℃ is (a) 0 cal/m² s (b) 20 cal/m²s (c) 40 cal/m²s (d) 80 cal/m²sarrow_forwardAn incandescent light bulb with a surface area of 0.0108 m2 and an emissivity of 0.87 has a surface temperature of 171.3°C. If the temperature of the surroundings are 21.2°C, what is the net rate of radiation heat transfer between the bulb and the surroundings? [round your final answer to one decimal place]? {o = 5.6704 x 10-8 W/(m²-K*)} 60 W T. S T surrarrow_forward
- A metal rod with a length of 50 cm and a cross-sectional area of 2.5 cm^2 is initially at a temperature of 20°C. If the rod absorbs 5000 joules of heat, what will be its final temperature? (The specific heat capacity of the metal is 0.4 J/(g°C), and the density is 8 g/cm^3.)arrow_forwardThe solar insolation at the top of the atmosphere is about 342 W/m^2. The total radiation absorbed at the surface of the Earth is 494 W/m^2. Explain how it is possible to absorb more radiation at the surface than comes in at the top of the atmosphere. (Answer should be one paragraph long)arrow_forwardA container used to store ice is made of wood 5.0 cm thick and has an effective area of 12,000 cm2 and thermal conductivity of 0.00027 cal/cm2-sec-°C/cm. How much ice inside the box would be melted each 24-hour day if the outside temperature is 25°C and the temperature inside the box is 5°C.provide solution with figure (fbd)arrow_forward
- For an isothermal layer, temperature is constant. Assume the scale height for the isothermal layer is 7.5 km, and surface pressure is 1000 hPa. What is the pressure at 20 km?arrow_forwardA window has dimensions of 1.65 m by 2.4 m and is made of glass 5.25 mm thick. On a winter day, the outside temperature is 22° C while the inside temperature is a comfortable at 17° C. (k of glass =0.085W/m.K) (1.5+1.5+2 = 5marks) Calculate the following: a) the area of the window in square metres b) the temperature gradient (AT/Ax)in kelvin/metre c) the rate of heat lost through the window by conduction in wattsarrow_forwardOn a summer day in Houston, the temperature is 20°C and the relative humidity is 74 percent. (a) What is the humidity? _________kg/m3(b) To what temperature could the air be cooled before condensation would start to take place? (That is, what is the dew point?)__________ °Carrow_forward
- The rate of heat transfer on a cold day in the Canada through a rectangular window is 2336 W. The temperature inside the home is 20.2 °C and the temperature outside the home is -7 °C. What is the area of the room if the thickness 6.7 mm and thermal conductivity value of 0.25 W/m/°C?arrow_forwardOn a day where the air temperature is 5.2 °C, the wind starts to blow, which increases the surface transfer co-efficient from 10 to 13.9 watts per metre-squared-Kelvin. For a human body with skin temperature 34°C and surface area 1.5 square metres, what is the wind-chill temperature? Answer: Checkarrow_forwardThe temperature and humidity in the valley in the early afternoon were 29 °C and 30%, respectively. Later, dry winds sweeping across the valley carried away 4.0 grams of water vapor from each cubic meter of air. The temperature during at that time had increased to 32 °C. What was the humidity (in %) then? Humidity vs Temperature Table is below: (°C) (g/ur) 10 9 16 13 21 18 24 22 29 30 32 35 14.3 16.7 12.3 O 16.0 O None of thesearrow_forward
- College PhysicsPhysicsISBN:9781305952300Author:Raymond A. Serway, Chris VuillePublisher:Cengage LearningUniversity Physics (14th Edition)PhysicsISBN:9780133969290Author:Hugh D. Young, Roger A. FreedmanPublisher:PEARSONIntroduction To Quantum MechanicsPhysicsISBN:9781107189638Author:Griffiths, David J., Schroeter, Darrell F.Publisher:Cambridge University Press
- Physics for Scientists and EngineersPhysicsISBN:9781337553278Author:Raymond A. Serway, John W. JewettPublisher:Cengage LearningLecture- Tutorials for Introductory AstronomyPhysicsISBN:9780321820464Author:Edward E. Prather, Tim P. Slater, Jeff P. Adams, Gina BrissendenPublisher:Addison-WesleyCollege Physics: A Strategic Approach (4th Editio...PhysicsISBN:9780134609034Author:Randall D. Knight (Professor Emeritus), Brian Jones, Stuart FieldPublisher:PEARSON