AP Notes, Outlines, Study Guides, Vocabulary, Practice Exams and more!

Atmospheric thermodynamics

Holt Earth Science Chapter 18, Section 18.1

Rating: 
0
No votes yet

Water?s Changes of State Water exists in all 3 states of matter and is made of hydrogen and oxygen atoms. In all 3 stages of matter, these molecules are in constant motion (higher temperature: more movement). Difference between 3 states is the arrangement of the water molecules. A. Ice, Liquid Water, and Water Vapor Ice is made of water molecules held together by mutual molecular attractions.They form a tight, orderly network and don?t move - they vibrate in a fixed position. When ice is heated, the molecules vibrate more, and when the rate of movement increases enough, the bonds between the molecules break, resulting in melting In the liquid state, the molecules are still tightly packed but move fast enough to slide past each other (this causes liquid water to be fluid)

Holt Earth Science Chapter 17, Section 17.4

Rating: 
0
No votes yet

Heating the Atmosphere A. What Happens to Incoming Solar Radiation? When radiation strikes an object, 3 things happen: some of the energy is absorbed by the object (converted to heat+temperature rises), some substances (water+air) are transparent to certain radiation wavelengths + transmit energy, and some radiation is bounced off the object without absorption/transmission. Reflection + scattering are responsible for redirected solar radiation. Out of the total solar radiation from the sun, 50% is absorbed by the land/sea, 20% is absorbed by the atmosphere/clouds, 5% is reflected from the land/sea surface, 5% is backscattered to space by the atmosphere, 20% is reflected by the clouds (in total, 30% is lost to space by reflection/scattering). B. Reflection and Scattering

Holt Earth Science Chapter 17, Section 17.2

Rating: 
0
No votes yet

Composition of the Atmosphere Air is a mixture of many discrete gases with their own physical properties in which different quantities of tiny solid/liquid particles are suspended. A. Major Components Composition of air varies depending on the time and place. If H20 Vapor, dust, and other variables were removed from the atmosphere, the makeup is very stable worldwide for an altitude of ~ 80 km. Ni and O2 make up 99% of clean, dry air. They are the most plentiful components, and important to life, but do not affect weather much. The remaining 1% is mostly Argon (0.93%) and other tiny quantities of many other gases. B. Carbon Dioxide (CO2)

Holt Earth Science Chapter 17, Section 17.1

Rating: 
0
No votes yet

Vertical Structure of the Atmosphere A. Pressure Changes Atmospheric Pressure: weight of the air above - at sea level, the avg. pressure ~ 1000 millibars (mb), or ~ 1 kg/cm2 Pressure at higher altitudes is less ? of the atmosphere is below 5.6 km (3.5 mi); at 16 km (10 mi), 90% of the atmosphere has been passed, and > 100 km (62 mi), only 0.00003 % of all gases in the atmosphere remain. Rest of atmosphere merges with space vacuum. B. Temperature Changes Near Earth?s surface, air temperature drops with an increase of height. I. Troposphere (air ?turns over?) Lowermost atmosphere layer (we live in here); temperature decreases with an altitude increase. All important weather occurs here.

IB Topic 3 problems set

Subject: 
Rating: 
0
No votes yet

Topic 3 ? Thermal physics Formative Assessment PROBLEM SET NAME: ________________________________ TEAM:__ THIS IS A PRACTICE ASSESSMENT. Show formulas, substitutions, answers, and units! Topic 3.1 ? Thermal concepts [ NGSS Supplement to Topic 3.1 begins at problem 51... ] The following questions are about internal energy. 1. What are the two forms of internal energy? 2. Suppose a liquid?s starting temperature is 20(C and its ending temperature is 35(C. Explain what happens to each form of internal energy. 3. How can you tell if the internal potential energy of a substance has changed? 4. How can you tell if the internal kinetic energy of a substance has changed? The following questions are about temperature scales.

Campbell Biology 9th Edition - Ch. 3 Water

Subject: 
Rating: 
0
No votes yet

Water is Special Polarity There are two types of covalent bonds, polar and nonpolar While nonpolar molecules share electrons equally, polar molecules do not. This results in one part of the molecule being partially positive and another part being partially negative. 2 Student Misconceptions and Concerns

ideal gas law

Subject: 
Rating: 
0
No votes yet
Tags: 

IDEAL GAS LAW THE REALTIONSHIP PV=nRT describes THE BEHAVIOR OF AN IDEAL GAS. (PRESSURE*VOLUME=#MOLES*R VALUE*TEMPERATURE)
Text automatically extracted from attachment below. Please download attachment to view properly formatted document.
---Extracted text from uploads/chemistry/ideal_gas_law.docx---

Gas Laws Notes

Subject: 
Rating: 
0
No votes yet

Gas Laws Properties of Gases Fluids Low density Highly compressible Completely fill a container and exert pressure in all directions Pressure the force exerted per unit of area Units of pressure: kilopascal (kPa) atmosphere (atm) torr (torr) millimeters of mercury (mmHg) pounds per square inch (psi) 1 atm = 760 mm Hg = 760 torr = 101 kPa Pressure and Volume How are pressure and volume of a gas related? Think about the demos yesterday. What are the words we use for this relationship? What would a graph look like? Pressure and Volume Boyle?s Law: the volume of a certain mass of gas at constant temperature is inversely proportional to the pressure applied to the gas P1V1 = P2V2 P V
Subscribe to RSS - Atmospheric thermodynamics

Need Help?

We hope your visit has been a productive one. If you're having any problems, or would like to give some feedback, we'd love to hear from you.

For general help, questions, and suggestions, try our dedicated support forums.

If you need to contact the Course-Notes.Org web experience team, please use our contact form.

Need Notes?

While we strive to provide the most comprehensive notes for as many high school textbooks as possible, there are certainly going to be some that we miss. Drop us a note and let us know which textbooks you need. Be sure to include which edition of the textbook you are using! If we see enough demand, we'll do whatever we can to get those notes up on the site for you!