A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags
Water temperature is a primary driver of stream ecosystems and commonly forms the basis of stream classifications. Robust models of stream temperature are critical as the climate changes, but estimating daily stream temperature poses several important challenges. We developed a statistical model tha...
| Published in: | PeerJ |
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| Main Authors: | , , , , , |
| Format: | Article |
| Language: | English |
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PeerJ Inc.
2016-02-01
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| Online Access: | https://peerj.com/articles/1727.pdf |
| _version_ | 1850119674485800960 |
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| author | Benjamin H. Letcher Daniel J. Hocking Kyle O’Neil Andrew R. Whiteley Keith H. Nislow Matthew J. O’Donnell |
| author_facet | Benjamin H. Letcher Daniel J. Hocking Kyle O’Neil Andrew R. Whiteley Keith H. Nislow Matthew J. O’Donnell |
| author_sort | Benjamin H. Letcher |
| collection | DOAJ |
| container_title | PeerJ |
| description | Water temperature is a primary driver of stream ecosystems and commonly forms the basis of stream classifications. Robust models of stream temperature are critical as the climate changes, but estimating daily stream temperature poses several important challenges. We developed a statistical model that accounts for many challenges that can make stream temperature estimation difficult. Our model identifies the yearly period when air and water temperature are synchronized, accommodates hysteresis, incorporates time lags, deals with missing data and autocorrelation and can include external drivers. In a small stream network, the model performed well (RMSE = 0.59°C), identified a clear warming trend (0.63 °C decade−1) and a widening of the synchronized period (29 d decade−1). We also carefully evaluated how missing data influenced predictions. Missing data within a year had a small effect on performance (∼0.05% average drop in RMSE with 10% fewer days with data). Missing all data for a year decreased performance (∼0.6 °C jump in RMSE), but this decrease was moderated when data were available from other streams in the network. |
| format | Article |
| id | doaj-art-233ee82ebeea4d91bece39f01ebc5d8f |
| institution | Directory of Open Access Journals |
| issn | 2167-8359 |
| language | English |
| publishDate | 2016-02-01 |
| publisher | PeerJ Inc. |
| record_format | Article |
| spelling | doaj-art-233ee82ebeea4d91bece39f01ebc5d8f2025-08-19T23:56:39ZengPeerJ Inc.PeerJ2167-83592016-02-014e172710.7717/peerj.1727A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lagsBenjamin H. Letcher0Daniel J. Hocking1Kyle O’Neil2Andrew R. Whiteley3Keith H. Nislow4Matthew J. O’Donnell5S.O. Conte Anadromous Fish Research Center, US Geological Survey/Leetown Science Center, Turners Falls, USAS.O. Conte Anadromous Fish Research Center, US Geological Survey/Leetown Science Center, Turners Falls, USAS.O. Conte Anadromous Fish Research Center, US Geological Survey/Leetown Science Center, Turners Falls, USADepartment of Environmental Conservation, University of Massachusetts, Amherst, USANorthern Research Station, USDA Forest Service, University of Massachusetts, Amherst, MA, USAS.O. Conte Anadromous Fish Research Center, US Geological Survey/Leetown Science Center, Turners Falls, USAWater temperature is a primary driver of stream ecosystems and commonly forms the basis of stream classifications. Robust models of stream temperature are critical as the climate changes, but estimating daily stream temperature poses several important challenges. We developed a statistical model that accounts for many challenges that can make stream temperature estimation difficult. Our model identifies the yearly period when air and water temperature are synchronized, accommodates hysteresis, incorporates time lags, deals with missing data and autocorrelation and can include external drivers. In a small stream network, the model performed well (RMSE = 0.59°C), identified a clear warming trend (0.63 °C decade−1) and a widening of the synchronized period (29 d decade−1). We also carefully evaluated how missing data influenced predictions. Missing data within a year had a small effect on performance (∼0.05% average drop in RMSE with 10% fewer days with data). Missing all data for a year decreased performance (∼0.6 °C jump in RMSE), but this decrease was moderated when data were available from other streams in the network.https://peerj.com/articles/1727.pdfStream temperatureEcologyAir temperatureStatistical modelClimate change |
| spellingShingle | Benjamin H. Letcher Daniel J. Hocking Kyle O’Neil Andrew R. Whiteley Keith H. Nislow Matthew J. O’Donnell A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags Stream temperature Ecology Air temperature Statistical model Climate change |
| title | A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags |
| title_full | A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags |
| title_fullStr | A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags |
| title_full_unstemmed | A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags |
| title_short | A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags |
| title_sort | hierarchical model of daily stream temperature using air water temperature synchronization autocorrelation and time lags |
| topic | Stream temperature Ecology Air temperature Statistical model Climate change |
| url | https://peerj.com/articles/1727.pdf |
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