Joshua Caster is a Geographer with the USGS Southwest Biological Science Center (SBSC), and the Grand Canyon Monitoring and Research Center (GCMRC), in Flagstaff, Arizona.
Joshua has experience conducting scientific investigations across a wide range of disciplines, including hydrology, hydrogeology, archaeology, geoarchaeology, geomorphology, biogeomorphology, and quaternary geology. His research interests focus on understanding past, present, and future landscape alterations within dryland ecosystems resulting from the changing environment and human activity. His current work with the Grand Canyon Monitoring and Research Center supports a variety of environmental and cultural resource management efforts within Grand Canyon National Park and other federal lands throughout the southwestern United States. Much of this work incorporates field-based investigations with remote sensing technology, including light detection and ranging (lidar) instruments, airborne and drone-based photography, and satellite imagery, to quantify terrestrial surface processes. He uses these technologies to characterize bio-physical interactions at millimeter to multi-kilometer scales for refining our understanding of how and why dryland landscapes are changing and the role management actions can play in altering landscape evolution.
Professional Experience
2014 – Present: Geographer, U.S. Geological Survey
Education and Certifications
In Progress: Ph.D., Earth Systems, Northern Arizona University
2010: M.S., Physical Geography, University of North Texas
Science and Products
Terrestrial lidar monitoring of the effects of Glen Canyon Dam operations on the geomorphic condition of archaeological sites in Grand Canyon National Park, 2010–2020
The influence of drying on the aeolian transport of river-sourced sand
Can we accurately estimate sediment budgets on Mars?
Biocrust and the soil surface: Influence of climate, disturbance, and biocrust recovery on soil surface roughness
Quantifying plant-soil-nutrient dynamics in rangelands: Fusion of UAV hyperspectral-LiDAR, UAV multispectral-photogrammetry, and ground-based LiDAR-digital photography in a shrub-encroached desert grassland
The effects of topographic surveying technique and data resolution on the detection and interpretation of geomorphic change
Quantifying and forecasting changes in the areal extent of river valley sediment in response to altered hydrology and land cover
The response of source-bordering aeolian dunefields to sediment-supply changes 1: Effects of wind variability and river-valley morphodynamics
The response of source-bordering aeolian dunefields to sediment-supply changes 2: Controlled floods of the Colorado River in Grand Canyon, Arizona, USA
Linking fluvial and aeolian morphodynamics in the Grand Canyon, USA
Modern landscape processes affecting archaeological sites along the Colorado River corridor downstream of Glen Canyon Dam, Glen Canyon National Recreation Area, Arizona
Geomorphic process from topographic form: automating the interpretation of repeat survey data in river valleys
Is timing really everything? Evaluating Resource Response to Spring Disturbance Flows
High-Flow Experiments on the Colorado River
Connectivity of Sand Resources Along the Colorado River in Grand Canyon
Soil surface properties and roughness data at two experimental restoration sites within the Southwestern USA
Geomorphic Change-Sediment Transport Data for the Little Colorado River, Arizona, USA
River Valley Sediment Connectivity Data, Colorado River, Grand Canyon
Meteorological Data for Selected Sites along the Colorado River Corridor, Arizona, 2014-2015
Geomorphic Process from Topographic FormData & Models
Science and Products
- Publications
Filter Total Items: 16
Terrestrial lidar monitoring of the effects of Glen Canyon Dam operations on the geomorphic condition of archaeological sites in Grand Canyon National Park, 2010–2020
The U.S. Geological Survey’s Grand Canyon Monitoring and Research Center, in coordination with the Glen Canyon Dam Adaptive Management Program, has monitored the geomorphic condition of select archaeological sites along the Colorado River in Grand Canyon using high-resolution terrestrial light detection and ranging (lidar) topographic surveys. Many of these sites are vulnerable to degradation by nAuthorsJoshua Caster, Joel B. Sankey, Helen Fairley, Alan KasprakThe influence of drying on the aeolian transport of river-sourced sand
Transgression and regression of water levels (stages) have impacted the evolution of aeolian landforms and sedimentary deposits throughout geologic history. We studied this phenomenon over a five-day period of reduced flow on the Colorado River in Grand Canyon National Park, AZ, USA, in March 2021. These transient low flows exposed river-channel sand deposits to the air, causing progressive desiccAuthorsJoel B. Sankey, Joshua Caster, Alan Kasprak, Helen C. FairleyCan we accurately estimate sediment budgets on Mars?
Sediment budgets are fundamentally important for planetary science. However, only one primary method, based on remote sensing, is currently available for determining extraterrestrial sediment budgets. For determining sediment budgets on Earth, both in-situ and remote sensing methods are available. Despite the widespread use of the two methods, there has been surprisingly little research on how welAuthorsJoel B. Sankey, Alan Kasprak, Matthew Chojnacki, Timothy N. Titus, Joshua Caster, Geoffrey DeBenedettoBiocrust and the soil surface: Influence of climate, disturbance, and biocrust recovery on soil surface roughness
Biocrust communities promote soil surface roughness, a key functional characteristic for soil ecology. However, the spatial scales at which biocrust communities contribute to surface roughness are not well understood. To refine our understanding of the spatial dynamics between biocrust and soil surface roughness, we used mm-resolution terrestrial LiDAR to measure micro-topographic roughness at sevAuthorsJoshua Caster, Temuulen T. Sankey, Joel B. Sankey, Matthew A. Bowker, Daniel Buscombe, Michael C. Duniway, Nichole Barger, Akasha M. Faist, Taylor JoyalQuantifying plant-soil-nutrient dynamics in rangelands: Fusion of UAV hyperspectral-LiDAR, UAV multispectral-photogrammetry, and ground-based LiDAR-digital photography in a shrub-encroached desert grassland
Rangelands cover 70% of the world's land surface, and provide critical ecosystem services of primary production, soil carbon storage, and nutrient cycling. These ecosystem services are governed by very fine-scale spatial patterning of soil carbon, nutrients, and plant species at the centimeter-to-meter scales, a phenomenon known as “islands of fertility”. Such fine-scale dynamics are challenging tAuthorsJoel B. Sankey, Temuulen T. Sankey, Junran Li, Sujith Ravi, Guan Wang, Joshua Caster, Alan KasprakThe effects of topographic surveying technique and data resolution on the detection and interpretation of geomorphic change
Change detection of high resolution topographic data is commonly used in river valleys to quantify reach- and site-scale sediment budgets by estimating the erosion/deposition volume, and to interpret the geomorphic processes driving erosion and deposition. Field survey data are typically collected as point clouds that are often converted to gridded raster datasets and the ultimate choice of grid rAuthorsAlan Kasprak, Nathaniel D. Bransky, Joel B. Sankey, Joshua Caster, Temulen T. SankeyQuantifying and forecasting changes in the areal extent of river valley sediment in response to altered hydrology and land cover
In river valleys, sediment moves between active river channels, near-channel deposits including bars and floodplains, and upland environments such as terraces and aeolian dunefields. Sediment availability is a prerequisite for the sustained transfer of material between these areas, and for the eco-geomorphic functioning of river networks in general. However, the difficulty of monitoring sediment aAuthorsAlan Kasprak, Joel B. Sankey, Daniel Buscombe, Joshua Caster, Amy E. East, Paul E. GramsThe response of source-bordering aeolian dunefields to sediment-supply changes 1: Effects of wind variability and river-valley morphodynamics
Source-bordering dunefields (SBDs), which are primarily built and maintained with river-derived sediment, are found in many large river valleys and are currently impacted by changes in sediment supply due to climate change, land use changes, and river regulation. Despite their importance, a physically based, applied approach for quantifying the response of SBDs to changes in sediment supply does nAuthorsJoel B. Sankey, Alan Kasprak, Joshua Caster, Amy E. East, Helen C. FairleyThe response of source-bordering aeolian dunefields to sediment-supply changes 2: Controlled floods of the Colorado River in Grand Canyon, Arizona, USA
In the Colorado River downstream of Glen Canyon Dam in the Grand Canyon, USA, controlled floods are used to resupply sediment to, and rebuild, river sandbars that have eroded severely over the past five decades owing to dam-induced changes in river flow and sediment supply. In this study, we examine whether controlled floods, can in turn resupply aeolian sediment to some of the large source-borderAuthorsJoel B. Sankey, Joshua Caster, Alan Kasprak, Amy E. EastLinking fluvial and aeolian morphodynamics in the Grand Canyon, USA
In river valleys, fluvial and upland landscapes are intrinsically linked through sediment exchange between the active channel, near-channel fluvial deposits, and higher elevation upland deposits. During floods, sediment is transferred from channels to low-elevation nearchannel deposits [Schmidt and Rubin, 1995]. Particularly in dryland river valleys, subsequent aeolian reworking of these flood depAuthorsAlan Kasprak, Sara G. Bangen, Daniel Buscombe, Joshua Caster, Amy E. East, Paul E. Grams, Joel B. SankeyModern landscape processes affecting archaeological sites along the Colorado River corridor downstream of Glen Canyon Dam, Glen Canyon National Recreation Area, Arizona
The landscape of the Colorado River through Glen Canyon National Recreation Area formed over many thousands of years and was modified substantially after the completion of Glen Canyon Dam in 1963. Changes to river flow, sediment supply, channel base level, lateral extent of sedimentary terraces, and vegetation in the post-dam era have modified the river-corridor landscape and have altered the effeAuthorsAmy E. East, Joel B. Sankey, Helen C. Fairley, Joshua J. Caster, Alan KasprakGeomorphic process from topographic form: automating the interpretation of repeat survey data in river valleys
The ability to quantify the processes driving geomorphic change in river valley margins is vital to geomorphologists seeking to understand the relative role of transport mechanisms (e.g. fluvial, aeolian, and hillslope processes) in landscape dynamics. High-resolution, repeat topographic data are becoming readily available to geomorphologists. By contrasting digital elevation models derived from rAuthorsAlan Kasprak, Joshua J. Caster, Sara G. Bangen, Joel B. Sankey - Science
Is timing really everything? Evaluating Resource Response to Spring Disturbance Flows
Glen Canyon Dam has altered ecological processes of the Colorado River in Grand Canyon. Before the dam was built, the Colorado River experienced seasonable variable flow rates, including springtime flooding events. These spring floods scoured the river bottom and enhanced natural processes that sustained the Colorado River ecosystem. Since the dam’s construction in 1963, springtime floods have...High-Flow Experiments on the Colorado River
Glen Canyon Dam has altered flow and fine sediment (sand, silt, and clay) dynamics of the Colorado River in Grand Canyon. Before the dam, the Colorado River experienced highly variable flows and carried a large amount of sediment through Grand Canyon, which maintained sandbars (highly valued camping areas in Grand Canyon) and provided sand that protected archeological and cultural sites from...Connectivity of Sand Resources Along the Colorado River in Grand Canyon
We study the links among different geomorphic processes that affect river valley landscapes in the Colorado River downstream from Glen Canyon Dam, Arizona. Dam-released flows affect the deposition and retention of sandbars that serve as sources for other sand resources, such as windblown sand dunes, throughout the Colorado River ecosystem. The degree to which the landscapes are differentially... - Data
Soil surface properties and roughness data at two experimental restoration sites within the Southwestern USA
This data release presents data used for analyzing spatial and temporal differences in soil surface roughness within selected biocrust communities. These records were collected by ground-based lidar for 121, 1m x 3m soil plots with biological soil crusts (biocrusts). Roughness was estimated from 5 mm resolution data (CloudCompare v. 2.10.2, 2019) for two Great Basin Desert sites (UTTR-1; UTTR-2) iGeomorphic Change-Sediment Transport Data for the Little Colorado River, Arizona, USA
These data were compiled to accompany flow modeling work on Little Colorado river above the mouth (USGS gage 09402300). The data include topographic data collected by LIDAR and total station in June 2017, high water marks from nine historic floods, and control points and gage structures. Topographic data include ground topography collected by LIDAR and channel bathymetry collected by total stationRiver Valley Sediment Connectivity Data, Colorado River, Grand Canyon
This workbook contains spatial data on the hydrology, sedimentology, and vegetation extent within the Colorado River corridor from 60 to 78 miles (97 to 125 kilometers) downstream from Glen Canyon Dam, Arizona. In combination with the accompanying MATLAB scripts, these data were used to generate the results within the accompanying manuscript (Kasprak et al., Quantifying and Forecasting Changes inMeteorological Data for Selected Sites along the Colorado River Corridor, Arizona, 2014-2015
This data release presents records collected from six automated weather stations in operation between January 1, 2014 and December 31, 2015 within the Colorado River Corridor of Grand Canyon National Park and Glen Canyon National Recreation Area. Data collection locations, equipment configurations and methods follow those of the original report (OFR 2014-1247). These files are 4-minute interval daGeomorphic Process from Topographic FormData & Models
The repeat topographic datasets used here are digital surface models (DSMs) derived using automated photogrammetry from photographs captured via aerial overflights during May 2002, 2009, and 2013. During overflights, discharge from Glen Canyon dam was held steady at 226 m3/s, and all subsequent analyses presented here apply to stages above this constant low flow discharge. DSMs are unique from tra - News