Peter Hartsough

ORCID: 0000-0001-7888-8028
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Plant Water Relations and Carbon Dynamics
  • Tree-ring climate responses
  • Cryospheric studies and observations
  • Hydrology and Watershed Management Studies
  • Soil Moisture and Remote Sensing
  • Geology and Paleoclimatology Research
  • Soil and Unsaturated Flow
  • Landslides and related hazards
  • Climate change and permafrost
  • Forest ecology and management
  • Climate variability and models
  • Groundwater and Isotope Geochemistry
  • Isotope Analysis in Ecology
  • Geophysical Methods and Applications
  • Soil erosion and sediment transport
  • Plant Pathogens and Fungal Diseases
  • Environmental and Cultural Studies in Latin America and Beyond
  • Precipitation Measurement and Analysis
  • Plant Pathogens and Resistance
  • Hydrology and Sediment Transport Processes
  • Seismic Waves and Analysis
  • Rangeland and Wildlife Management
  • Atmospheric and Environmental Gas Dynamics
  • Advanced Computational Techniques and Applications
  • Enhanced Oil Recovery Techniques

University of California, Davis
2010-2022

Plant (United States)
2017

University of Nevada, Reno
2001-2010

Desert Research Institute
2001-2004

United States Geological Survey
2003

New Mexico Institute of Mining and Technology
2003

Washington State University
2003

A large reservoir of bioavailable nitrogen (up to approximately 10(4) kilograms per hectare, as nitrate) has been previously overlooked in studies global distribution. The accumulating subsoil zones arid regions throughout the Holocene. Consideration raises estimates vadose-zone inventories by 14 71% for warm deserts and shrublands worldwide 3 16% globally. Subsoil nitrate accumulation indicates long-term leaching from desert soils, impelling further evaluation nutrient dynamics xeric...

10.1126/science.1086435 article EN Science 2003-11-06

Using data from a water‐balance instrument cluster with spatially distributed sensors we determined the magnitude and within‐catchment variability of components catchment‐scale water balance, focusing on relationship seasonal evapotranspiration to changes in snowpack soil moisture storage. Co‐located, continuous snow depth measurements were deployed rain–snow transition catchment mixed‐conifer forest Southern Sierra Nevada. At each elevation placed open, under canopy, at drip edge both...

10.2136/vzj2011.0001 article EN Vadose Zone Journal 2011-08-01

ABSTRACT The conversion of bedrock to regolith marks the inception critical zone processes, but factors that regulate it remain poorly understood. Although thickness and degree weathering are widely thought be important regulators development its water‐storage potential, functional relationships between properties processes generate documented. This is due in part fact difficult characterize by direct observations over broad scales needed for process‐based understanding zone. Here we use...

10.1002/esp.3502 article EN Earth Surface Processes and Landforms 2013-11-08

Enhanced understanding of subsurface water storage will improve prediction future impacts climate change, including drought, forest mortality, wildland fire, and strained security. Previous research has examined the importance plant‐accessible in soil, but upland landscapes within Mediterranean climates, soil often accounts for only a fraction storage. We draw insights from previous case study Southern Sierra Critical Zone Observatory to define attributes storage; review observed patterns...

10.1002/wat2.1277 article EN Wiley Interdisciplinary Reviews Water 2018-02-15

Mountain runoff ultimately reflects the difference between precipitation (P) and evapotranspiration (ET), as modulated by biogeophysical mechanisms that intensify or alleviate drought impacts. These modulating are seldom measured not fully understood. The impact of warm 2012-15 California on heavily instrumented Kings River basin provides an extraordinary opportunity to enumerate four controlled mountain hydrology. Two intensified impact: (i) evaporative processes have first access local...

10.1038/s41598-017-19007-0 article EN cc-by Scientific Reports 2018-01-08

Weathering in the critical zone causes volumetric strain and mass loss, thereby creating subsurface porosity that is vital to overlying ecosystems. We used geochemical geophysical measurements quantify relative importance of loss---the physical chemical components porosity---in weathering granitic saprolite southern Sierra Nevada, California, USA. Porosity decrease with depth imply more than doubles volume during exhumation surface by erosion. Chemical depletion relatively uniform,...

10.1126/sciadv.aao0834 article EN cc-by-nc Science Advances 2019-09-06

Core Ideas Water quality and stream flow have temporal spatial trends in response to variable climate. Our work reveals how Sierra Nevada forests responded recovered from multiyear drought. Regolith thickness reveal water storage capacity differences with elevation. Monitoring shows deep‐water changes via plant utilization or capillary during Sensor networks within the Southern Critical Zone Observatory (SSCZO) Kings River Experimental Watersheds (KREW) document cycle spanning west slope of...

10.2136/vzj2018.04.0081 article EN cc-by-nc-nd Vadose Zone Journal 2018-01-01

Abstract The water balance is an essential tool for hydrologic studies and quantifying water‐balance components the focus of many research catchments. A fundamental question remains regarding appropriateness closure assumptions when not all are available. In this study, we leverage in‐situ measurements fluxes storage from Southern Sierra Critical Zone Observatory (SSCZO) Kings River Experimental Watersheds (KREW) to investigate annual errors across large (1016–5389 km 2 ) river basins small...

10.1002/hyp.14199 article EN Hydrological Processes 2021-04-30

Cellulose delta18O and deltaD can provide insights on climates hydrological cycling in the distant past how these factors differ spatially. However, most studies of plant cellulose have used only one isotope, commonly delta18O, resulting difficulties partitioning variation precipitation vs. evaporative conditions that affect leaf water isotopic enrichment. Moreover, observations pronounced diurnal differences from conventional steady-state model predictions fractionation cast some doubt...

10.1890/13-0988.1 article EN Ecological Applications 2013-10-28

The relationship between wood growth and environmental variability at the tropical treeline of North America was investigated using automated, solar-powered sensors (a meteorological station two dendrometer clusters) installed on Nevado de Colima, Mexico (19° 35' N, 103° 37' W, 3,760 m a.s.l.). Pure stands Pinus hartwegii Lindl. (Mexican mountain pine) were targeted because their suitability for tree-ring analysis in low-latitude, high-elevation, American Monsoon environments. Stem size...

10.3390/s100605827 article EN cc-by Sensors 2010-06-09

Abstract Subsurface weathering has traditionally been measured using cores and boreholes to quantify vertical variations in weathered material properties. However, these measurements are typically available at only a few, potentially unrepresentative points on hillslopes. Geophysical surveys, conversely, span many more and, as shown here, can be used obtain representative, site‐integrated perspective subsurface weathering. Our approach aggregates data from multiple seismic refraction surveys...

10.1029/2020gl088322 article EN Geophysical Research Letters 2020-07-17

Abstract Large uncertainty remains in the spatial distribution of deep soil organic carbon (OC) storage and how climate controls belowground OC. This research aims to quantify OC stocks, characterize age chemical composition, evaluate climatic impacts on from surface through critical zone bedrock. These objectives were carried out at four sites along a bio-climosequence Sierra Nevada, California. On average, 74% was stored below A horizon, up 30% saprock (friable weakly weathered bedrock)....

10.1088/1748-9326/ac3bfe article EN cc-by Environmental Research Letters 2021-11-23

Site‐specific numerical modeling of four sites in two arid alluvial basins within the Nevada Test Site employs a conceptual model deep system hydrodynamics that includes vapor transport, role xeric vegetation, and long‐term surface boundary transients. Surface sequences, spanning 110 kyr, best reproduce measured chloride concentration matric potential profiles from (230–460 m) boreholes concur with independent paleohydrologic paleoecological records region. Simulations constrain pluvial...

10.1029/2001wr000825 article EN Water Resources Research 2002-12-01

We present here the 2001–2004 results of observational field studies aimed at quantifying tropical timberline climate and radial increment Pinus hartwegii Lindl. trees on Nevado de Colima, in middle North American Monsoon region. An automated weather station was installed 3760 m a.s.l., 19°34.778′N latitude, 103°37.180′W longitude, within a forest where multi-century tree-ring records had been previously developed. At same time, electronic sensors for recording tree growth 30-min intervals...

10.1657/1523-0430(2005)037[0016:dwatga]2.0.co;2 article EN Arctic Antarctic and Alpine Research 2005-02-01

Monitoring the snow pack is crucial for many stakeholders, whether hydro-power optimization, water management or flood control. Traditional forecasting relies on regression methods, which often results in melt runoff predictions of low accuracy non-average years. Existing ground-based real-time measurement systems do not cover enough physiographic variability and are mostly installed at elevations. We present hardware software design a state-of-the-art distributed Wireless Sensor Network...

10.3390/s17112583 article EN cc-by Sensors 2017-11-09

A 14.6 kyr chronology of infiltration developed from deep vadose (unsaturated) zone cores in southern Nevada is presented to assess the nitrogen loss active rooting zone. Soil water chemistry first used develop a paleohydrology and subsequently fluxes. While elevated concentrations (as NO 3 ) are commonly found desert zones, /Cl ratios indicate that nitrate behaved conservatively beneath Mean fluxes root range 103 108 mg/m²/yr appear relatively constant over time, spite dramatic climate...

10.1029/2000gl011823 article EN Geophysical Research Letters 2001-08-01

Abstract To provide complementary information on the hydrologically important rain–snow-transition elevation in mountain basins, this study provides two estimation methods using ground measurements from basin-scale wireless sensor networks: one based wet-bulb temperature T wet and other snow-depth of accumulation ablation. With data 17 spatially distributed clusters (178 nodes) networks, American Feather River basins California’s Sierra Nevada, we analyzed transition during 76 storm events...

10.1175/jhm-d-20-0028.1 article EN Journal of Hydrometeorology 2020-08-18

We investigated the seasonal variation in pools of water available to mature trees growing at high elevation a tropical environment. The study focused on dominant tree species (Pinus hartwegii) about 3800 m a.s.l. Nevado de Colima, Mexico, where climate is typical North American Monsoon System. Stable isotope ratios hydrogen and oxygen extracted from soil, xylem, leaves were measured through cycle two dry wet seasons 2003–2004. Isotopic also accumulated precipitation, few single...

10.1657/1523-0430(06-117)[hartsough]2.0.co;2 article EN Arctic Antarctic and Alpine Research 2008-05-01

Forests at risk to diseases caused by invasive Phytophthora pathogens can be grouped into two broad classes: those already invaded the focal pathogen where disease has emerged or significant of invasion and subsequent emergence disease. This dichotomy represents distinct management scenarios – treating after before emerges with a set epidemiological, ecological, practical characteristics that determine optimal actions associated costs. Here we present initial outcomes from experiments aimed...

10.5399/osu/fp.7.1.4021 article EN Forest Phytophthoras 2017-01-01

Core Ideas Biotite content was positively related to regolith thickness in granitic terrain. Depth regulates transformations by dampening subsurface temperature. The degree of soil development does not reflect deep characteristics. We evaluated the effects temperature and subtle differences lithology (biotite content) on pedogenesis (soils + saprock) terrain southern Sierra Nevada. Deep sampled from summit backslope landscape positions two catchments representing transition rain‐dominated...

10.2136/sssaj2018.03.0120 article EN publisher-specific-oa Soil Science Society of America Journal 2019-03-01

Abstract This study reports on a blending approach using snowpack measurements from wireless‐sensor network, gauge precipitation, and atmospheric‐moisture data to estimate mountain precipitation amount phase. We applied the in California's American River basin, dense network consisting of over 130 sensor nodes distributed across upper, more snow‐dominated part basin (≥1,500 m elevation). Analysis 60 events water years 2014–2017 showed that provides estimates orographic enhancement reduce...

10.1029/2021wr029954 article EN Water Resources Research 2022-05-01

Abstract Understanding potential response of forest carbon (C) and nutrient storage to warming is important for climate mitigation policies. Unfortunately, those responses are difficult predict in seasonally dry forests, part, because ecosystem processes highly sensitive both changes temperature precipitation. We investigated how might alter stocks C, nitrogen (N), phosphorus (P) vegetation the entire regolith (soil + weathered bedrock or “saprock”) using a space‐for‐time substitution along...

10.1029/2022gb007429 article EN cc-by-nc Global Biogeochemical Cycles 2022-11-01
Coming Soon ...