Probabilistic estimates of the distribution of near-surface (within 1m) permafrost in Alaska.

• Main Authors: Neal J. Pastick, Bruce K. Wylie, M. Torre Jorgenson, Shawn J. Nield, Kristofer D. Johnson, Andrew O. Finley
• Format: Dataset
• Language: unknown
• Published: USGS Science Data Catalog 2015
• Subjects: Permafrost; Spatial Modeling; Pedometrics; Remote Sensing; Alaska; Ice; permafrost
• Online Access: https://search.dataone.org/view/8dfb8200-d07f-4784-ae0d-60713d9bb214

This medium resolution (i.e. 30-m pixels) spatial dataset provides an estimate of the occurrence of near-surface (within 1 m of the ground surface) permafrost in Alaska. The dataset was developed using a decision-tree model that statistically and spatially extended late-season field observations (n ~ 17,000) using remotely sensed imagery, climatic data, and thematic maps of a wide range of surface and subsurface biophysical characteristics. To circumvent the use of seasonal frost observations, only thaw-depth measurements taken during late-season months (late July to mid-September) or measurements designated to have no near-surface (within 1m) permafrost were used for model calibration and validation. Individual pixel values represent the probability of encountering near-surface permafrost (i.e. 0 to 100 %), as derived from a tree ensemble model, and pixel values greater than 100 correspond to masked land cover types (i.e. 101 = open water; 102 = perennial ice/snow; 103 = developed; 104 = barren, and; 105 = cultivated areas) as defined by the 2001 National Land Cover Database. Decision tree models and resultant maps were tested using independent field observations and f-fold cross validations, which indicated that the map product has an overall accuracy of approximately 85 % when using a probability threshold of 50 % (i.e. less than 50 % = near-surface permafrost absent; greater than or equal to 50 % = near-surface permafrost present).