Water is universally critical for life on earth, and snowmelt plays an essential role in the hydrologic cycle, contributing up to 75% of water supply in much of the western United States. As a result, estimating the timing and magnitude of snowmelt is an integral water resources challenge; snow surface temperature observations are key to this issue. It is well established that snow melts at 0°C, so frequent snow temperature measurements supply crucial information for evaluating snowmelt. However, few ground observations of snow surface temperature are available, and those that are only represent a small area. By measuring infrared radiation, satellite thermal imaging can remotely determine surface temperature over large areas and time scales where ground observations are sparse or nonexistent. However, this imagery is limited by its coarse spatial resolution, which results in a blurring of temperatures across study regions. This challenge is especially prevalent for mixed pixels, or pixels with varied land surfaces such as a mix of snow and vegetation or changing topography. Thus, this project investigates how well satellite imaging represents snow surface temperature. Airborne thermal imagery were acquired by the UW Applied Physics Laboratory over Yosemite National Park, California, coincident with ASTER satellite imagery on 21 April 2017. I apply methods including data analysis and zonal statistics over the study area in order to compare finer resolution airborne imaging to coarser resolution satellite imagery. Furthermore, I calculate characteristics of land variation to evaluate where satellite imagery can be scaled for more accurate results. This project works towards the implementation of satellite thermal infrared for use in snow models, creating new datasets for hydrologists to more effectively plan our water resources.