OPhO 2020, Открит кръг — Задача 34. Global Warming
2020 Online Physics Olympiad (OPhO): Open Contest v1.5 · 25 май 2020 г.
2020 Online Physics Olympiad (OPhO): Open Contest v1.5
OPhO Lead Organizers and Writers: Adithya Balachandran, Eddie Chen, Ashmit Dutta, Ethan Hu, Viraj Jayam, Rishab Parthasarathy, Kushal Thaman, Max Wang, QiLin Xue
OPhO Website Developer: Ben Oommen
Advisors: Dr. Branislav Kisačanin, Kye Shi, Kevin Zhou
Указания
If you wish to request a clarification, please use this form. To see all clarifications, see this document.
- Use in this contest. See the constants sheet on the following page for other constants.
- This test contains 55 short answer questions. Each problem will have three possible attempts.
- The weight of each question depends on our scoring system found here. Put simply, the later questions are worth more, and the overall amount of points from a certain question decreases with the number of attempts and days that you take to solve a problem as well as the number of teams who solve it. This means that your score decreases with the number of tries and days you take to solve a given problem.
- Any team member is able to submit an attempt. Choosing to split up the work or doing each problem together is up to you. Note that after you have submitted an attempt, your teammates must refresh their page before they are able to see it.
- Answers should contain at least three significant figures, unless otherwise specified. All answers within the 1% range will be accepted.
- When submitting a response using scientific notation, please use exponential form. In other words, if your answer to a problem is , please type into the submission portal.
- A standard scientific or graphing handheld calculator may be used. Technology and computer algebra systems like Wolfram Alpha or the one in the TI nSpire will not be needed. Attempts to use these tools will be classified as cheating.
- You are allowed to use Wikipedia or books in this exam. Asking for help on online forums or your teachers will be considered cheating and may result in a possible ban from future competitions.
- Top scorers from this contest will qualify to compete in the Online Physics Olympiad Invitational Contest, which is an olympiad-style exam. More information will be provided to invitational qualifiers after the end of the Open Contest.
- In general, answer in SI units (meter, second, kilogram, watt) unless otherwise specified. Please answer all questions in degrees unless otherwise specified.
- If the question asks to give your answer as a percent and your answer comes out to be “”, please input the value into the submission form.
- Do not put letters in your answer on the submission portal! If your answer is “ meters” , input only the value into the submission portal.
- Do not communicate information to anyone else apart from your team-members before the exam ends on May 29, 2020 at 11:59 PM UTC.
List of Constants
Proton mass,
Neutron mass,
Electron mass,
Avogadro’s constant,
Universal gas constant,
Boltzmann’s constant,
Electron charge magnitude,
1 electron volt,
Speed of light,
Universal Gravitational constant,
Acceleration due to gravity,
1 unified atomic mass unit,
Planck’s constant,
Permittivity of free space,
Coulomb’s law constant,
Permeability of free space,
Magnetic constant,
1 atmospheric pressure,
Wien’s displacement constant,
Stefan-Boltzmann constant,
Условие
Life on Earth would not exist as we know it without the atmosphere. There are many reasons for this, but one of which is temperature. Let’s explore how the atmosphere affects the temperature on Earth. Assume that all thermal energy striking the earth uniformly and ideally distributes itself across the Earth’s surface.
- Assume that the Earth is a perfect black body with no atmospheric effects. Let the equilibrium temperature of Earth be . (The sun outputs around , and is away.)
- Now assume the Earth’s atmosphere is isothermal. The short wavelengths from the sun are nearly unaffected and pass straight through the atmosphere. However, they mostly convert into heat when they strike the ground. This generates longer wavelengths that do interact with the atmosphere. Assume that the albedo of the ground is 0.3 and , the emissivity and absorptivity of the atmosphere, is 0.8. Let the equilibrium average temperature of the planet now be .
What is the percentage increase from to ?
Note: The emissivity is the degree to which an object can emit longer wavelengths (infrared) and the absorptivity is the degree to which an object can absorb energy. Specifically, the emissivity is the ratio between the energy emitted by an object and the energy emitted by a perfect black body at the same temperature. On the other hand, the absorptivity is the ratio of the amount of energy absorbed to the amount of incident energy.
Отговори
289.601 K
The problem asks for the percentage increase from to ; the official solution boxes only the temperature and prints no percentage.
Решение
Solution: Let us solve this problem in the case of the Earth being a graybody first and then substitute values for when it is a blackbody. The portion of energy that reaches the Earth is given by the ratio between the cross-sectional area of the satellite and the area of an imaginary sphere centered around the sun with a radius of . Thus, the incoming radiation is multiplied by a factor of . The energy from the sun that the surface absorbs is , where is the energy output of the sun. Here as the sphere encompassing will be 4 times the area of its intercept.
We can now write two systems of equations at the atmosphere and the ground of the Earth. At the top of the atmosphere, we require equilibrium meaning that zero net radiation leaves the atmosphere or:
Similarly, at the ground, we write another equilibrium equation of:
Thus, solving the ground equilibrium equation yields us and plugging back into the atmosphere equilibrium equation tells us:
Оригинал в Архива: open.pdf · официални решения: open_sol.pdf