Award Abstract # 1802714
Collaborative Proposal: MSB-FRA: Scaling Climate, Connectivity, and Communities in Streams

NSF Org: DEB
Division Of Environmental Biology
Recipient: REGENTS OF THE UNIVERSITY OF CALIFORNIA, THE
Initial Amendment Date: August 6, 2018
Latest Amendment Date: June 11, 2021
Award Number: 1802714
Award Instrument: Standard Grant
Program Manager: Matthew Kane
mkane@nsf.gov
 (703)292-7186
DEB
 Division Of Environmental Biology
BIO
 Directorate for Biological Sciences
Start Date: January 1, 2019
End Date: September 30, 2024 (Estimated)
Total Intended Award Amount: $252,362.00
Total Awarded Amount to Date: $421,691.00
Funds Obligated to Date: FY 2018 = $252,362.00
FY 2021 = $169,329.00
History of Investigator:
  • Albert RUHI (Principal Investigator)
    albert.ruhi@berkeley.edu
Recipient Sponsored Research Office: University of California-Berkeley
1608 4TH ST STE 201
BERKELEY
CA  US  94710-1749
(510)643-3891
Sponsor Congressional District: 12
Primary Place of Performance: University of California-Berkeley
130 Mulford Hall #3114
Berkeley
CA  US  94720-3114
Primary Place of Performance
Congressional District:
12
Unique Entity Identifier (UEI): GS3YEVSS12N6
Parent UEI:
NSF Program(s): MacroSysBIO & NEON-Enabled Sci
Primary Program Source: 01001819DB NSF RESEARCH & RELATED ACTIVIT
01002122DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 097Z, 102Z, 7959
Program Element Code(s): 795900
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.074

ABSTRACT

Half of the Earth's streams are intermittent: they occasionally dry or stop flowing. Since the 1980s, researchers who study streams have developed theories about how stream ecosystems work. Each theory is different, but they all focus on a single physical aspect of streams that is thought to best explain how stream ecosystem structure and function vary from one place to another. Physical factors that have been considered include stream size, floods, and climate. However, the body of work informing the development of these theories, and the body of work supporting them, is based on research from streams that flow continuously, or "perennial streams." Given that half of the Earth's streams are intermittent, there is a need to develop a new theory for streams that explains how drying acts as a control on stream ecosystem structure and function, how intermittent and perennial streams are different, and how those differences vary from region to region. This project uses macrosystems ecology as a foundation to develop and test such a theory that can be applied to all the Earth's streams. A smartphone app will map wet and dry stream reaches in conjunction with international research partners (1000 Intermittent Rivers Project), and citizen science organizers, and educational partners to create new teaching tools. The research may help inform decisions on water use where streams and intermittent and human populations are increasing. Seven graduate student will be included on the diverse research team.

This research project is comprised of three components. The first is a three-year field study of intermittent and continuously flowing streams in 10 different regions across the southern, central, and western US led by researchers at five different US universities that will collect streamflow and biological data. The field study will be focused on investigating how macroinvertebrate communities in intermittent and perennial streams differ in species composition and abundance, and how these differences vary according to climate. In 9 of the 10 regions, the researchers will use National Ecological Observatory Network (NEON) collected data, and sampling will follow NEON sampling protocols to generate NEON-compatible data. The second component will develop fine-scale hydrological models of the study watersheds using the Coupled Routing and Excess STorage (CREST) model. These models will predict where and when streams dry in these watersheds, and researchers will model streamflow patterns under different scenarios related to sea surface temperature oscillations and other changes. The third component of the project will generate spatial models that integrate the empirically collected ecological data in the field with the hydrological model outputs. This part of the project will investigate how large-scale climate oscillations (e.g. El Nino Southern Oscillation) influence regional drying patterns differently, and how shifts in spatial drying patterns influence stream ecosystems.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Gill, Brian A and Allen, Daniel C and Mims, Meryl C and Neeson, Thomas M and Ruhi, Albert and Atkinson, Carla L and Shogren, Arial J and Apgar, Travis M and Compson, Zacchaeus G and Cook, Stephen and Trumbo, Daryl R and Busch, Michelle H and Hollien, Kels "Combined benthic and stream edge sampling better represent macroinvertebrate assemblages than benthic sampling alone along an aridity gradient" Limnology and Oceanography: Methods , v.22 , 2024 https://doi.org/10.1002/lom3.10601 Citation Details
Leathers, Kyle and Herbst, David and Safeeq, Mohammad and Ruhi, Albert "Dynamic, downstreampropagating thermal vulnerability in a mountain stream network: Implications for biodiversity in the face of climate change" Limnology and Oceanography , v.68 , 2022 https://doi.org/10.1002/lno.12264 Citation Details
Palmer, Margaret and Ruhi, Albert "Linkages between flow regime, biota, and ecosystem processes: Implications for river restoration" Science , v.365 , 2019 10.1126/science.aaw2087 Citation Details
Sarremejane, Romain and Stubbington, Rachel and England, Judy and Sefton, Catherine E. M. and Eastman, Michael and Parry, Simon and Ruhi, Albert "Drought effects on invertebrate metapopulation dynamics and quasiextinction risk in an intermittent river network" Global Change Biology , v.27 , 2021 https://doi.org/10.1111/gcb.15720 Citation Details

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The drying of rivers is becoming increasingly common, but impacts of drying on river ecosystems are not well understood. Previous research has shown that drying is harmful to many species but can be beneficial to some–altering the composition of species found at a given site (i.e., the local communities). However, effects of river drying on biodiversity and ecosystem processes at larger spatial scales, e.g., by altering processes such as dispersal and phenology along the river network, remain largely unknown. Further, the consequences of drying may be mediated by climate, but past studies have rarely compared drying impacts across gradients of aridity. This project sought to examine the effects of drying on stream ecosystems across multiple levels of biological organization (from genes to ecosystems), and to understand how differences in drying effects may be influenced by climatic context. Project team members examined streamflow, aquatic invertebrate communities, and genetic diversity in ten watersheds throughout the United States over the span of three years. Research led by the Ruhi Lab at UC Berkeley focused on how invertebrate communities potentially linked by dispersal (or metacommunities) change over time in response to stream drying. Specifically, we sought to understand when, where, and why drying alters the local and regional processes that generate and support riverine biodiversity. 

 

In addition to collecting samples of aquatic invertebrates at Pinnacles National Park (Chalone Creek) and in California’s Sierra Nevada (Kings River Experimental Watersheds), our team developed time series analysis and mathematical simulations to test how species respond to a wide range of drying conditions. To date, the project has produced seven peer-reviewed publications, with further papers in development. Main findings led by our group relate to the importance of river drying location (e.g., in headwaters vs. in main river reaches), showing that location, combined with drying severity and extent, determines river biodiversity not just at small (local) spatial scales, but across entire watersheds (Ruhi et al., in prep). We also found that drought can synchronize dynamics of species across large spatial scales, increasing their aggregate extinction risk (Sarremejane et al 2021, Global Change Biology). Further, we showed that thermal vulnerability quickly propagates across the stream network, and that air temperature in Sierra Nevada streams has the greatest influence on water temperature in the late spring and summer, when air and water temperatures peak and organisms are more likely to be stressed (Leathers et al. 2023, Limnology & Oceanography). Understanding how drying may lead to different ecological outcomes (e.g., depending on the geographic context) can help inform and prioritize conservation efforts at the watershed scale. More broadly, work funded by this project has enabled the development of scientific frameworks that connect change in hydrology to changes in species dynamics and ecosystem processes (Palmer & Ruhi 2019, Science). 

 

Two graduate students, two postdocs, and ten undergraduates were trained through the project resulting in career advancement and graduation. We have also collaborated with Pinnacles National Park to take over groundwater monitoring operations, lead outreach to the public in events like the California Biodiversity Week, and share our research with the public while in the field. The scholarship generated by this award is enabling further downstream science and helping connect scientific advances to river conservation and restoration practices—many of which address the pressing need to anticipate ecosystem responses to drought and flow intermittency.

 


Last Modified: 03/12/2025
Modified by: Albert RUHI

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