To understand how water changes phase within the atmosphere and within a snowpack, we need to understand basic chemistry and molecular physics. Popular Science video with ads on growing snowflakes with Ken Libbrecht
We may not have a lab of this quality, but you can print and build your own hexogonal snow crystal out of paper.
Download the lab and data files to your computer. Then, upload them to your JupyterHub following the instructions here. Note, if you took CEWA 565 Data Analysis Class or are otherwise already familiar with Python, you can skip Lab 1-1 and go to Lab 1-2.
Some extra helpful activities:
In this homework assignment we will work start with programming and data visualization to better qualitatively understand the types of datasets that we'll be using the rest of the quarter. This homework is on the shorter side because we have a fieldtrip next week and will also be covering the material necessary for the second homework. Please download the notebooks at the top of this page and use them as reference for your coding. Be sure to save your work for later reference
For this week's homework, we will pretend we are in very controlled laboratory conditions. If you dislike python, these questions can all be answered with pencil, paper, and a calculator, but you may want to use this exercise as a chance to practice your programming skills.
A. Imagine you have a 1 cubic centimeter block of ice at -10 degrees C and 1 atm of pressure. Calculate the amount of energy required to melt all of the ice. (Note that you will have to warm it to 0 degrees C before you begin melting it.)
B. Now, consider that same block of ice at -10 degrees C and 1 atm of pressure. Calculate the amount of energy required to sublimate all of the ice. (Note that you do not need to warm the ice to sublimate it.)
C. Repeat the calculations above, but imagine you are high in the mountains at 0.5 atm of pressure. What changes?
D. We know that cold snow is primarily a mixture of ice and air. Consider no phase changes and temperatures between -15 degrees and -5 degrees C. Imagine that no interactions occur between the ice and air in the snow matrix. How does the energy required to heat the mixture those 10 degrees change as the fractions of ice vs. air change in the total mixture?
E. I argue that sublimation saves the snowpack more than it reduces it. Why would I say this? Do you agree or disagree? Use the specific and latent heats in lab 1-2 to make your argument.