LPMLE <i>n</i> –A Frequency Domain Method to Estimate Vertical Streambed Fluxes and Sediment Thermal Properties in Semi‐Infinite and Bounded Domains-Reference-Cited by-同舟云学术

LPMLE n –A Frequency Domain Method to Estimate Vertical Streambed Fluxes and Sediment Thermal Properties in Semi‐Infinite and Bounded Domains

Published:2022-03 Issue:3 Volume:58 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resources Research

Author:

van Kampen Ricky¹²^ORCID,Schneidewind Uwe³^ORCID,Anibas Christian⁴^ORCID,Bertagnoli Andrea⁵^ORCID,Tonina Daniele⁵^ORCID,Vandersteen Gerd⁶^ORCID,Luce Charles⁷^ORCID,Krause Stefan³^ORCID,van Berkel Matthijs¹^ORCID

Affiliation:

1. DIFFER—Dutch Institute for Fundamental Energy Research Eindhoven The Netherlands

2. Department of Mechanical Engineering Control Systems Technology Group Eindhoven University of Technology Eindhoven The Netherlands

3. School of Geography Earth and Environmental Sciences University of Birmingham Birmingham UK

4. School of Civil and Environmental Engineering Water Research Laboratory UNSW Sydney Sydney NSW Australia

5. Center for Ecohydraulics Research University of Idaho Boise ID USA

6. Department ELEC Vrije Universiteit Brussel Brussels Belgium

7. US Forest Service Boise ID USA

Funder

H2020 Euratom

Deutsche Forschungsgemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021WR030886

Reference57 articles.

1. Using multi-tracer inference to move beyond single-catchment ecohydrology

2. From streambed temperature measurements to spatial-temporal flux quantification: using the LPML method to study groundwater-surface water interaction

3. Delineation of spatial-temporal patterns of groundwater/surface-water interaction along a river reach (Aa River, Belgium) with transient thermal modeling

4. Active heat pulse sensing of 3-D-flow fields in streambeds

5. Using high-resolution distributed temperature sensing to quantify spatial and temporal variability in vertical hyporheic flux

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