4 Data
The analysis utilizes three main types of satellite data from Google Earth Engine and one self uploaded shapefile:
4.1 Study Area
Center point: Mount Everest (86.9252°E, 27.98833°N)
Analysis buffer: 10-15km radius
Includes multiple climbing routes (shapefile import from private asset)
var routes = ee.FeatureCollection("projects/ee-wbwhaha/assets/Everest");4.2 Temperature Data
Source:
- MODIS MOD11A2 dataset
Temporal resolution: 8-day composite
Spatial resolution: 1km
Time period: February 18, 2011 - March 30, 2025
Variables:
- Daytime Land Surface Temperature (LST_Day_1km)
- Nighttime Land Surface Temperature (LST_Night_1km)
Data processing:
- For more LST algorithms details (here)[https://lpdaac.usgs.gov/documents/119/MOD11_ATBD.pdf]. \[ \text{Temperature (°C)} = \text{Raw Value} \times 0.02 - 273.15 \]
4.3 Terrain Data
Source:
- USGS/SRTMGL1_003 dataset
- NASA/NASADEM_HGT/001 dataset
Spatial resolution: 30m
Variables:
- DEM (the elevation data)
- Slope (identifying steep areas >20 degrees, calculated from DEM)
- Aspect (terrain orientation, calculated from DEM)
Data processing:
- For each route, the system creates a line geometry
- Along this line, 100 equidistant points are sampled
- At each point, the elevation value is extracted from the DEM
- The resulting elevation values are stored as a feature property
4.4 Snow Cover Data
Source:
- Sentinel-2 imagery
Temporal resolution: 5-10 days (depending on satellite overpasses)
Spatial resolution: 10m (Bands 3, 4, 8) and 20m (Band 11)
Time period: January 2015 - Present
Variables:
- Band 3 (Green): Used in NDSI calculation to detect snow
- Band 11 (SWIR): Used in NDSI calculation to detect snow
- Snow Class: Derived from the NDSI and snow fraction (classified into 4 categories: < 25%, 25–50%, 50–75%, > 75% snow cover)
Data processing:
NDSI is calculated using the formula: \[ \text{NDSI} = \frac{\text{Band 3} - \text{Band 11}}{\text{Band 3} + \text{Band 11}} \]
Snow fraction is calculated using a neighborhood mean reducer over a 10-pixel radius
Snow cover classes are derived by categorizing the snow percentage into four classes