Abstract

In the headwater catchments of the Rocky Mountains, plant productivity and its dynamics are largely dependent upon water availability, which is influenced by changing snowmelt dynamics associated with climate change. Understanding and quantifying the interactions between snow, plants and soil moisture is challenging, since these interactions are highly heterogeneous in mountainous terrain, particularly as they are influenced by microtopography within a hillslope. Recent advances in satellite remote sensing have created an opportunity for monitoring snow and plant dynamics at high spatiotemporal resolutions that can capture microtopographic effects. In this study, we investigate the relationships among topography, snowmelt, soil moisture and plant dynamics in the East River watershed, Crested Butte, Colorado, based on a time series of 3-meter resolution PlanetScope normalized difference vegetation index (NDVI) images. To make use of a large volume of high-resolution time-lapse images (17 images total), we use unsupervised machine learning methods to reduce the dimensionality of the time lapse images by identifying spatial zones that have characteristic NDVI time series. We hypothesize that each zone represents a set of similar snowmelt and plant dynamics that differ from other identified zones and that these zones are associated with key topographic features, plant species and soil moisture. We compare different distance measures (Ward and complete linkage) to understand the effects of their influence on the zonation map. Results show that the identified zones are associated with particular microtopographic features; highly productive zones are associated with low slopes and high topographic wetness index, in contrast with zones of low productivity, which are associated with high slopes and low topographic wetness index. The zones also correspond to particular plant species distributions; higher forb coverage is associated with zones characterized by higher peak productivity combined with rapid senescence in low moisture conditions, while higher sagebrush coverage is associated with low productivity and similar senescence patterns between high and low moisture conditions. In addition, soil moisture probe and sensor data confirm that each zone has a unique soil moisture distribution. This cluster-based analysis can tractably analyze high-resolution time-lapse images to examine plant-soil-snow interactions, guide sampling and sensor placements and identify areas likely vulnerable to ecological change in the future.

Highlights

  • In the Rocky Mountains, water availability during the growing season is the primary limiting factor for plant productivity, impacted by snow accumulation and snowmelt timing [1,2,3]

  • We hypothesize that such snow- and plant dynamics-based zones are indicative of belowground soil moisture dynamics and that once we identify such zones, we can use this information to optimize soil moisture measurements and to understand the spatiotemporal variability in soil moisture and plant dynamics

  • We evaluated whether the normalized difference vegetation index (NDVI) time series is suitable for clustering by computing the Hopkin’s statistic

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Summary

Introduction

In the Rocky Mountains, water availability during the growing season is the primary limiting factor for plant productivity, impacted by snow accumulation and snowmelt timing [1,2,3]. Methods for capturing the spatiotemporal variability of soil moisture include electromagnetic point measurements such as time domain reflectometry (TDR), capacitance and time domain transmission sensors [9]. Such measurements are costly and time-consuming, requiring either a soil moisture sensor network or significant human labor for sufficiently dense and extensive manual sampling [9]. Microwave-based satellite technologies have been developed to map near-surface soil moisture While these technologies have been successfully demonstrated, their resolution is low, with footprints on the order of tens of kilometers [10]. The spatial scale of these datasets, which ranges from 20 meters for Sentinel to 500 meters for the Moderate Resolution Imaging Spectrometer (MODIS), presents a limitation for investigating the impact of soil moisture on plants because plant, soil and topographic features can vary significantly across a few meters [7,8,13,14,15]

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