Long-term trajectories of fractional component change in the Northern Great Basin, USA

Matthew B. Rigge; Hua Shi; Collin Homer; Patrick Danielson; Brian J. Granneman

doi:10.1002/ecs2.2762

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Long-term trajectories of fractional component change in the Northern Great Basin, USA

Matthew B. Rigge·Hua Shi·Collin Homer·Patrick Danielson·Brian J. Granneman

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Abstract

The need to monitor change in sagebrush steppe is urgent due to the increasing impacts of climate change, shifting fire regimes, and management practices on ecosystem health. Remote sensing provides a cost effective and reliable method for monitoring change through time and attributing changes to drivers. We report an automated method of mapping rangeland fractional component cover over a large portion of the northern Great Basin from 1986 to 2016 using a dense Landsat imagery time-series. Our method improved upon the traditional change vector method by considering the legacy of change at each pixel. We evaluate cover trends stratified by climate bin and assess spatial and temporal relationships with climate variables. Finally, we statistically evaluate the minimum time density needed to accurately characterize temporal patterns and relationships with climate drivers. Over the 30-year period shrub cover declined and bare ground increased. While few pixels had > 10% cover change, a large majority had at least some change. All fractional components had significant spatial relationships with water year precipitation (WYPRCP), maximum temperature (WYTMAX), and minimum temperature (WYTMIN) in all years. Shrub and sagebrush cover in particular respond positively to warming WYTMIN, resulting from the largest increases in WYTMIN being in the coolest and wettest areas, and negatively to warming WYTMAX since the largest increases in WYTMAX are in the warmest and driest areas. The trade-off of lowering temporal density against removing cloud-contaminated years is justified as temporal density appears to have only a modest impact on trends and climate relationships until n ≤ 6, but multi-year gaps are proportionally more influential. Gradual change analysis is likely to be less sensitive to n than abrupt change. These data can be used to answer critical questions regarding the influence of climate change and the suitability of management practices.

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Source-reported bounding extent: 34.59704151614417° to 44.15068115978094° latitude; -122.56347656249999° to -109.248046875° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Matthew B. Rigge, Hua Shi, Collin Homer, Patrick Danielson, Brian J. Granneman. 2019-06-03. Long-term trajectories of fractional component change in the Northern Great Basin, USA. https://doi.org/10.1002/ecs2.2762

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