As a research hydrologist and geomorphologist, my previous research has generally followed two trajectories: 1) geomorphic response to disturbance including dam removal, surface coal mining, and invasive species and 2) characterizing patterns and controls on flow permanence of intermittent and ephemeral rivers and streams.
My current focus includes broadening flow permanence research to the Pacific Northwest region and evaluating changes in sediment and stream water temperature regimes and associated implications on river ecosystem health in Pacific Northwest mountain rivers
Professional Experience
Research Hydrologist, USGS Washington Water Science Center, Tacoma, WA (2015-Present)
Assistant Professor, Ohio State University, Ohio Agricultural Research and Development Center (OARDC), Wooster, OH (2012-2015)
Postdoctoral Fellow, School of Aquatic and Fishery Sciences, University of Washington, Seattle, WA (2010-2012)
Education and Certifications
Ph.D. Fluvial Geomorphology, Colorado State University, 2009
M.A. Forest Hydrology, University of Washington, 2004
B.A. Biology, Colorado College, 1998
Science and Products
Updated classifications of flow permanence on streams in the Colville National Forest
State of the Science in Streamflow Modeling in the North Central Region to Address Partner Needs for Water Availability Under Drought Conditions
Drought preparedness in Mt. Rainier National Park
Development of a Streamflow Data Catalog and Evaluation of the Vulnerability of Sensitive Fish Species to Climate Change Across the Pacific Northwest
Quantifying suspended-sediment load and transport characteristics in the Calawah and Upper Bogachiel Rivers, Washington
Coarse sediment delivery and routing in the White River
Fine sediment infiltration in Chinook spawning gravels in the Sauk River Basin, Washington
Geomorphology & Sediment Transport
Probability of Streamflow Permanence (PROSPER)
Sauk River Sediment
Supporting data for and predictions from streamflow permanence modeling in Mount Rainier National Park and surrounding area, Washington, 2018-2020
Suspended-Sediment Data for the Bogachiel and Calawah Rivers, WA for Water Years 2019-2021
Supporting Spatial Data for Sediment Studies in the Bogachiel and Calawah River Watersheds, Washington
Supporting data for streamflow permanence studies in the Huachuca Mountains, Arizona, 2010-2014.
Supporting data for and predictions from streamflow permanence modeling in Mt. Rainier National Park and surrounding area, Washington, 2018-2020
FLOwPER Database: StreamFLOw PERmanence field observations, April 2020 - Nov 2020
Suspended Sediment and Water Temperature Data in the Suiattle River and the Downey Creek Tributary, Washington for select time periods over 2013 - 2017
Supporting Data for Sediment Studies in the White River Watershed
FLOwPER Database: StreamFLOw PERmanence field observations, August 2019 - October 2019
Stream metabolism models for the Regional Stream Quality Assessments of the National Water Quality Program, 2013 to 2016
Predicting probabilities of late summer surface flow presence in a glaciated mountainous headwater region
Changes in suspended-sediment yields under divergent land-cover disturbance histories: A comparison of two large watersheds, Olympic Mountains, USA
High resolution spatiotemporal patterns of flow at the landscape scale in montane non-perennial streams
Predictions and drivers of sub-reach-scale annual streamflow permanence for the upper Missouri River basin: 1989-2018
How does precipitation variability control bedload response across a mountainous channel network in a maritime climate?
Relative contributions of suspended sediment between the upper Suiattle River Basin and a non-glacial tributary, Washington, May 2016–September 2017
Assessing climate change impacts on Pacific salmon using bioenergetics and spatiotemporal explicit river temperature predictions under varying riparian conditions
Managing nonperennial headwater streams in temperate forests of the United States
Most rivers and streams run dry every year
Beyond streamflow: Call for a national data repository of streamflow presence for streams and rivers in the United States
Identifying geomorphic process domains in the synthetic landscapes of West Virginia, USA
Coarse sediment dynamics in a large glaciated river system: Holocene history and storage dynamics dictate contemporary climate sensitivity
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
Updated classifications of flow permanence on streams in the Colville National Forest
The Issue: Streamflow permanence refers to the probability that a stream will lose surface flow (become a dry channel), as well as the timing, duration, and frequency of drying. Patterns of streamflow permanence drive important decisions regarding forest management and other land uses. The Colville National Forest Land and Resource Management Plan (2019), for example, specifies riparian management...State of the Science in Streamflow Modeling in the North Central Region to Address Partner Needs for Water Availability Under Drought Conditions
Land and water managers often rely on hydrological models to make informed management decisions. Understanding water availability in streams, rivers, and reservoirs during high demand periods that coincide with seasonal low flows can affect how water managers plan for its distribution for human consumption while sustaining aquatic ecosystems. Substantial advancement in hydrological modeling has ocDrought preparedness in Mt. Rainier National Park
The Issue: Water supply for park operations and backcountry users is determined by the spatial extent of perennial streams in Mount Rainier National Park (MORA). In addition, the presence or absence of streamflow (flow permanence) is related to water temperature, which influences the occurrence and distribution of aquatic species including cold-water fishes and insects. Information about the...Development of a Streamflow Data Catalog and Evaluation of the Vulnerability of Sensitive Fish Species to Climate Change Across the Pacific Northwest
As freshwater streams and native fish are threatened by changing environmental conditions, efforts to coalesce existing data and integrate modeling and projection tools are increasingly necessary for informing effective land, water, and species management. For example, identifying and integrating disparate datasets of streamflow, stream water temperature and species distribution is critical for deQuantifying suspended-sediment load and transport characteristics in the Calawah and Upper Bogachiel Rivers, Washington
The issue: Salmonid fisheries are an important cultural and economic activity and efforts to support a thriving fisheries industry remain a major priority for the Quileute Tribe on the Olympic Peninsula, Washington. Land use changes can have a profound influence on basin sediment production with direct effects on fisheries (Madej and Ozaki, 2009). Studies are needed to improve estimates of the...Coarse sediment delivery and routing in the White River
The Issue: Ongoing channel aggradation has reduced flow conveyance along the lower White River, increasing the flood risk in urban-suburban areas. A refined understanding of the delivery, transport and deposition of sediment in the White River, and how those processes may be influenced by climate and existing dam operations, is necessary in order to plan for future flood hazard in the lower White...Fine sediment infiltration in Chinook spawning gravels in the Sauk River Basin, Washington
The Issue: There is concern that inherently high finer-grained (small gravel, sand, and silt) sediment loads in the Sauk River system may adversely affect egg-to-fry survival of ESA-listed Chinook salmon in the Sauk River and lower Skagit River Basin. However, there are no quantitative data for the Sauk River basin to assess if fine sediment deposition and infiltration into spawning gravels are at...Geomorphology & Sediment Transport
Geomorphology is the study of the formation and evolution of landforms on Earth's surface. In the Pacific Northwest, volcanoes, tectonic movement, glaciers, rain, snow, wind, vegetation, animals, and people all shape the landscape at different scales of time and space. Of particular interest in the region is the form and processes of rivers, a branch of the science termed fluvial geomorphology...Probability of Streamflow Permanence (PROSPER)
PRObability of Streamflow PERmanence (PROSPER) Rivers and streams are constantly changing. Streamflows can change throughout the year and between years due to snowmelt, precipitation, diversions, and return flows. For many streams, these fluctuations determine whether a stream has year-round flow or not. PROSPER is a project initiated to better understand what causes these fluctuations in...Sauk River Sediment
Fine-grained sediments in the lower reach of the Sauk River are adversely affecting the health and spawning of Chinook salmon. Climate change and forestry practices have been proposed as suspected causes of a reported increase in sediment loading to the river. To determine the amount and timing of suspended-sediment loading to the river and possible connections to adverse effects on Chinook salmon... - Data
Supporting data for and predictions from streamflow permanence modeling in Mount Rainier National Park and surrounding area, Washington, 2018-2020
This data release contains spatially gridded geospatial data (rasters), R scripts, and supporting files to run Random Forest models to predict the probability of late summer surface flow in Mount Rainier and surrounding area in Washington State for 2018–20. Gridded geospatial data that describes the physical conditions of Mount Rainier National Park and surrounding area are used to refine the exisSuspended-Sediment Data for the Bogachiel and Calawah Rivers, WA for Water Years 2019-2021
This data release summarizes suspended sediment monitoring results on the Bogachiel (USGS 12042800) and Calawah (USGS 12043000) Rivers between water years 2019 and 2021, based on a combination of continuous turbidity monitoring and discrete suspended-sediment concentration (SSC) measurements. Data and results for each monitoring station were combined into zip files. Each zip file contains: SummSupporting Spatial Data for Sediment Studies in the Bogachiel and Calawah River Watersheds, Washington
This Data Release provides spatial data to support analysis of land cover change and channel width change in the Bogachiel and Calawah River basins, Washington. This supports a larger analysis that quantifies suspended-sediment yields for the two basins for water years 1977-1978 and more recently, for water years 2019-2021. Collectively the study evaluates influences of hydrology, geology, fire, aSupporting data for streamflow permanence studies in the Huachuca Mountains, Arizona, 2010-2014.
This Data Release provides supporting data to characterize and identify influences of streamflow permanence in headwater streams in the Huachuca Mountains, Arizona, U.S.A. Relative conductivity as a proxy for surface water presence was measured in headwater streams in the Huachuca Mountains from 2010-2014. These data are summarized as mean daily values. Geologic influences on the timing of surfaceSupporting data for and predictions from streamflow permanence modeling in Mt. Rainier National Park and surrounding area, Washington, 2018-2020
This data release contains spatially gridded geospatial data (rasters), R scripts, and supporting files to run Random Forest models to predict the probability of late summer surface flow in Mt. Rainier and surrounding area in Washington State for 2018?20. Gridded geospatial data that describes the physical conditions of Mt. Rainier National Park and surrounding area are used to refine the existingFLOwPER Database: StreamFLOw PERmanence field observations, April 2020 - Nov 2020
IMPORTANT NOTE: This dataset includes spatial locations where streamflow permanence observations (continuous flow, discontinuous flow, and dry) were recorded using the FLOwPER (FLOw PERmanence) field survey available in the Survey 123 and S1 mobile application. Additional information to describe the field conditions are included as part of the survey. Field observations in the FLOwPER Database havSuspended Sediment and Water Temperature Data in the Suiattle River and the Downey Creek Tributary, Washington for select time periods over 2013 - 2017
This data release provides suspended-sediment (concentration and load) and water temperature data for two locations along the Suiattle River (USGS 1217900 and 12188380) and a tributary, Downey Creek (USGS 1217985) in Washington State for partial periods over 2013-2017. Suspended-sediment and water temperature data were collected over two summer seasons from May through September 2016 and 2017 at USupporting Data for Sediment Studies in the White River Watershed
The White River is a dynamic gravel-bedded system in western Washington, with headwaters on Mount Rainier. Chronic aggradation in the lower river has reduced flood conveyance to a point where modest discharges are increasingly causing substantial flood damage. In order to better understand the dynamics governing this aggradation, and how aggradation rates may be influenced by forecasted changes inFLOwPER Database: StreamFLOw PERmanence field observations, August 2019 - October 2019
IMPORTANT NOTE: More recent versions of these data release are available at this link. This dataset includes spatial locations where streamflow permanence observations (continuous flow, discontinuous flow, and dry) were recorded using the FLOwPER (FLOw PERmanence) field survey available in the Survey 123 and S1 mobile application. Additional information to describe the field conditions are includStream metabolism models for the Regional Stream Quality Assessments of the National Water Quality Program, 2013 to 2016
This dataset provides details from stream metabolism models for 20 stream sites in the United States that were sampled as part of the National Water Quality Program's Regional Stream Quality Assessments (RSQA). Metabolism was estimated at each site using the streamMetabolizer package in R. For each of the 20 sites, three files are provided; (1) the input data, which includes continuous dissolved o - Publications
Filter Total Items: 21
Predicting probabilities of late summer surface flow presence in a glaciated mountainous headwater region
Accurate mapping of streams that maintain surface flow during annual baseflow periods in mountain headwater streams is important for informing water availability for human consumption and is a fundamental determinant of in-channel conditions for stream-dwelling organisms. Yet accurate mapping that captures local spatial variability and associated local controls on surface flow presence is limited.AuthorsKristin Jaeger, Roy Sando, Sarah B. Dunn, Andrew S. GendaszekChanges in suspended-sediment yields under divergent land-cover disturbance histories: A comparison of two large watersheds, Olympic Mountains, USA
Improvements in timber harvest practices and reductions in harvest volumes over the past half century are commonly presumed to have reduced sediment loads in many western US rivers. However, direct assessments in larger watersheds are relatively sparse. Here, we compare 2019–21 sediment concentrations against those of the late 1970s in the Bogachiel and Calawah River watersheds, adjacent and simiAuthorsKristin Jaeger, Scott W. Anderson, Sarah B. DunnHigh resolution spatiotemporal patterns of flow at the landscape scale in montane non-perennial streams
Intermittent and ephemeral streams in dryland environments support diverse assemblages of aquatic and terrestrial life. Understanding when and where water flows provide insights into the availability of water, its response to external controlling factors, and potential sensitivity to climate change and a host of human activities. Knowledge regarding the timing of drying/wetting cycles can also beAuthorsRomy Sabathier, Michael Bliss Singer, John C Stella, Dar A. Roberts, Kelly K. Caylor, Kristin Jaeger, Julian OldenPredictions and drivers of sub-reach-scale annual streamflow permanence for the upper Missouri River basin: 1989-2018
The presence of year-round surface water in streams (i.e., streamflow permanence) is an important factor for identifying aquatic habitat availability, determining the regulatory status of streams, managing land use change, allocating water resources, and designing scientific studies. However, accurate, high resolution, and dynamic prediction of streamflow permanence that accounts for year-to-yearAuthorsRoy Sando, Kristin Jaeger, William H. Farmer, Theodore B. Barnhart, Ryan R. McShane, Toby L. Welborn, Kendra E. Kaiser, Konrad Hafen, Kyle W. Blasch, Benjamin C. York, Alden ShallcrossHow does precipitation variability control bedload response across a mountainous channel network in a maritime climate?
Modeled stream discharge is often used to drive sediment transport models across channel networks. Because sediment transport varies non-linearly with flow rates, discharge modeled from daily total precipitation distributed evenly over 24-hrs may significantly underestimate actual bedload transport capacity. In this study, we assume bedload transport capacity determined from a hydrograph resultingAuthorsJeffrey Keck, Erkan Istanbulluoglu, Jessica Lundquist, Christina Bandaragoda, Kristin Jaeger, Guillaume S. Mauger, Alex Horner-DevineRelative contributions of suspended sediment between the upper Suiattle River Basin and a non-glacial tributary, Washington, May 2016–September 2017
Concentrations of suspended sediment were measured in discrete samples and turbidity was continuously monitored at four U.S. Geological Survey streamgages in western Washington State, including one gage on the Sauk River; two gages on the Suiattle River, a tributary to the Sauk River; and one gage on Downey Creek, a tributary to the Suiattle River. The Suiattle River is a sediment-rich stream withAuthorsKristin L. Jaeger, Scott W. Anderson, Craig A. Senter, Christopher A. Curran, Scott MorrisAssessing climate change impacts on Pacific salmon using bioenergetics and spatiotemporal explicit river temperature predictions under varying riparian conditions
Pacific salmon and trout populations are affected by timber harvest, the removal and alteration of riparian vegetation, and the resulting physical changes to water quality, temperature, and associated delivery of high-quality terrestrial prey. Juvenile salmon and trout growth, a key predictor of survival, is poorly understood in the context of current and future (climate-change mediated) conditionAuthorsAndrew Spanjer, Andrew S. Gendaszek, Elyse J. Wulfkuhle, Robert W. Black, Kristin JaegerManaging nonperennial headwater streams in temperate forests of the United States
Forest management guidelines are designed to protect water quality from unintended effects of land use changes such as timber harvest, mining, or forest road construction. Although streams that periodically cease to flow (nonperennial) drain the majority of forested areas, these streams are not consistently included in forest management guidelines. This paper reviews management guidelines for nonpAuthorsStephanie K. Kampf, Kathleen Dwyer, Matthew P. Fairchild, Jason B. Dunham, Craig D. Snyder, Kristin Jaeger, Charles H. Luce, John C. Hammond, Codie Wilson, Margaret Zimmer, Marielle SidellMost rivers and streams run dry every year
The flowing waters of surface rivers and streams efficiently transport sediment, organic material and nutrients, among other things, from hillsides and overland areas to downstream lakes, reservoirs and the ocean. Along the way, rivers and streams (hereafter referred to collectively as streams) provide important resources for our communities and support rich, complex ecosystems. Non-perennial streAuthorsKristin JaegerBeyond streamflow: Call for a national data repository of streamflow presence for streams and rivers in the United States
Observations of the presence or absence of surface water in streams are useful for characterizing streamflow permanence, which includes the frequency, duration, and spatial extent of surface flow in streams and rivers. Such data are particularly valuable for headwater streams, which comprise the vast majority of channel length in stream networks, are often non-perennial, and are frequently the mosAuthorsKristin Jaeger, Konrad Hafen, Jason B. Dunham, Ken M. Fritz, Stephanie K. Kampf, Theodore B. Barnhart, Kendra E. Kaiser, Roy Sando, Sherri L Johnson, Ryan R. McShane, Sarah Beth DunnIdentifying geomorphic process domains in the synthetic landscapes of West Virginia, USA
Human activities such as mining, agriculture, and urbanization have resulted in severe, large‐scale alteration to landform organization and associated geomorphic processes. The mountaintop mining (MTM) region of West Virginia, USA has experienced dramatic topographic alteration, by removing steep slopes and introducing plateau‐like areas at ridgelines and benches on valley fills. The resulting engAuthorsKristin Jaeger, Matthew V RossCoarse sediment dynamics in a large glaciated river system: Holocene history and storage dynamics dictate contemporary climate sensitivity
The gravel-bedded White River drains a 1279 km2 basin in Washington State, with lowlands sculpted by continental glaciation and headwaters on an actively glaciated stratovolcano. Chronic aggradation along an alluvial fan near the river’s mouth has progressively reduced flood conveyance. In order to better understand how forecasted climate change may influence coarse sediment delivery and aggradatiAuthorsScott W. Anderson, Kristin JaegerNon-USGS Publications**
Costigan, K.H., K.L. Jaeger, C.W. Goss, K.M. Fritz, and P.C. Goebel, 2016, "Understanding controls on flow permanence in intermittent rivers to aid ecological research: Integrating meteorology, geology and land cover." Ecohydrology. DOI:10.1002/2015WR017601Costigan, K.H., P.J. Soltesz, and K.L. Jaeger, 2015, “Large wood in Central Appalachian headwater streams: Controls on and potential changes to wood loads from infestation of hemlock woolly adelgid,” Earth Surface Processes and Landforms. DOI: 10.1002/esp.3751Jaeger K.L., 2015, “Reach-scale geomorphic differences between headwater streams draining mountaintop mined and unmined catchments.” Geomorphology 236:25-33. DOI: 10.1016/j.geomorph.2015.02.007Schriever T.A., M.T. Bogan, K.S. Boersma, M. Cañedo-Argüelles, K.L. Jaeger, J.D. Olden, and D.A. Lytle, 2015, “Hydrology shapes taxonomic and functional structure of desert stream invertebrate communities,” Freshwater Science doi: 10.1086/680518
Jaeger K.L., J.D. Olden, and N.D. Pelland, 2014, “Climate change poised to threaten hydrologic connectivity and endemic fishes in dryland streams,” Proceedings of the National Academy of Sciences, USA 111: 13894-13899. Doi:10.1073/pnas.1320890111
Jaeger K.L. and J.D. Olden, 2012, “Electrical resistance sensor arrays as a means to quantify longitudinal connectivity of rivers,” River Research and Applications 28:1843-1852. DOI: 10.1002/rra.1554
Jaeger K.L. and E.E. Wohl, 2011, “Channel response in a semiarid stream to removal of tamarisk and Russian olive,” Water Resources Research 47: W02536 doi: 10.1029/2009WR008741.
Jaeger K.L., E.E. Wohl, and A. Simon, 2010, “A comparison of average rates of alluvial erosion between the southwestern and southeastern United States,” Earth Surface Processes and Landforms, 35: 447–459. DOI: 10.1002/esp.1960Wohl E.E. and K.L. Jaeger, 2009, “Geomorphic implications of hydroclimatic differences among step-pool channels,” Journal of Hydrology 374: 148-161. DOI: 10.1016/j.jhydrol.2009.06.008
Cadol D.C., E.E. Wohl, J.G. Goode, and K.L. Jaeger, 2009, “Wood distribution in forested headwater streams of La Selva, Costa Rica,” Earth Surface Processes and Landforms 34:1198-1215. DOI: 10.1002/esp.1800**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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