Abstract

Mountains of the arid Great Basin region of Nevada are home to critical water resources and numerous species of plants and animals. Understanding the nature of climatic variability in these environments, especially in the face of unfolding climate change, is a challenge for resource planning and adaptation. Here, we utilize an Embedded Sensor Network (ESN) to investigate landscape-scale temperature variability in Great Basin National Park (GBNP). The ESN was installed in 2006 and has been maintained during uninterrupted annual student research training expeditions. The ESN is comprised of 29 Lascar sensors that record hourly near-surface air temperature and relative humidity at locations spanning 2000 m and multiple ecoregions within the park. From a maximum elevation near 4000 m a.s.l. atop Wheeler Peak, the sensor locations are distributed: (1) along a multi-mountain ridgeline to the valley floor, located ~2000 m lower; (2) along two streams in adjoining eastern-draining watersheds; and (3) within multiple ecological zones including sub-alpine forests, alpine lakes, sagebrush meadows, and a rock glacier. After quality checking all available hourly observations, we analyze a twelve-year distributed temperature record for GBNP and report on key patterns of variability. From 2006 to 2018, there were significantly increasing trends in daily maximum, minimum and mean temperatures for all elevations. The average daily minimum temperatures increased by 2.1°C. The trend in daily maximum temperatures above 3500 m was significantly greater than the increasing trends at lower elevations, suggesting that daytime forcings may be driving enhanced warming at GBNP’s highest elevations. These results indicate that existing weather stations, such as the Wheeler Peak SNOTEL site, alone cannot account for small-scale variability found in GBNP. This study offers an alternative, low-cost methodology for sustaining long-term, distributed observations of conditions in heterogeneous mountainous environments at finer spatial resolutions. In arid mountainous regions with vulnerable water resources and fragile ecosystems, it is imperative to maintain and extend existing networks and observations as climate change continues to alter conditions.

Highlights

  • Great Basin National Park (GBNP) comprises a mid-latitude, semi-arid mountain landscape, where sharp vertical gradients underscore the vitality of water access and where biophysical indicators record the impacts of past and present climate change on Park ecosystems (Porinchu et al, 2007; Reinemann et al, 2009)

  • Based on the results of the relative calibration and drift study we found non-significant sensor drift had taken place within the Embedded Sensor Network (ESN) and results were within manufacturer specifications

  • This study demonstrates that ESN data are both reliable and consistent with expected local near-surface temperature conditions, providing new insights into temperature variability and change within GBNP

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Summary

Introduction

Great Basin National Park (GBNP) comprises a mid-latitude, semi-arid mountain landscape, where sharp vertical gradients underscore the vitality of water access and where biophysical indicators record the impacts of past and present climate change on Park ecosystems (Porinchu et al, 2007; Reinemann et al, 2009). The topography is shaped by regional uplift and extensional tectonics dating to the Cenozoic that resulted in N-S faulting up-thrusted mountain ranges bounding flat valleys characteristic of the “Basin and Range” landscape, wherein Nevada contains the largest number of mountain ranges of all States in the United States (Dickinson, 2006). Concerns for this region and ongoing climate changes center on the vertically distributed biodiversity and available ecosystem services, water. There is a noticeable imprint of human intervention in the regional hydrology as intensifying groundwater use and a proposed pipeline to transport groundwater from the Snake Valley aquifers to rapidly expanding urban development in Las Vegas comprises a legal transboundary apportionment precedent (Hall and Cavataro, 2013; Masbruch, 2019)

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