Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent
Abstract In this study, the regional tree‐ring chronology of Picea crassifolia was used to estimate annual (September to August) streamflow of the Shiyang River for the period from AD 1765 to 2010. The linear regression model was stable and could explain 41.5% of the variance for the calibration per...
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crwiley:10.1002/hyp.10788 2024-06-02T08:11:31+00:00 Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent Chen, Feng Yuan, Yu‐jiang Zhang, Rui‐bo Wang, Hui‐qin Shang, Hua‐ming Zhang, Tong‐wen Qin, Li Fan, Zi‐ang National Basic Research Program of China Meteorology Public Welfare Industry Research Special Project Basic Research Operating Expenses of the Central-level Non-profit Research Institutes China Desert Meteorological Science Research Foundation 2016 http://dx.doi.org/10.1002/hyp.10788 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10788 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10788 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 30, issue 13, page 2211-2222 ISSN 0885-6087 1099-1085 journal-article 2016 crwiley https://doi.org/10.1002/hyp.10788 2024-05-03T10:46:05Z Abstract In this study, the regional tree‐ring chronology of Picea crassifolia was used to estimate annual (September to August) streamflow of the Shiyang River for the period from AD 1765 to 2010. The linear regression model was stable and could explain 41.5% of the variance for the calibration period of 1955–2005. According to the streamflow reconstruction, dry periods with below average streamflow occurred in AD 1775–1804, 1814–1823, 1831–1856, 1862–1867, 1877–1885, 1905–1910, 1926–1932, 1948–1951, 1960–1963 and 1989–2002. Periods of relatively wet years are identified for AD 1765–1774, 1805–1813, 1824–1830, 1857–1861, 1868–1876, 1886–1904, 1911–1925, 1933–1947, 1952–1959, 1964–1988 and 2003–2010. Comparisons with the precipitation reconstructions from surrounding areas supplied a high degree of confidence in our reconstruction. Our reconstructed streamflow is significantly correlated with sea surface temperature in the eastern equatorial Pacific Ocean and the North Atlantic Ocean. The Multitaper spectral and correlation analyses also suggested that the reconstructed streamflow variation in the Shiyang River could be associated with large‐scale atmospheric‐oceanic variability, such as El Niño‐Southern Oscillation (ENSO). The linkages among the streamflow reconstruction, NAO and ENSO suggest the connection of regional streamflow variations to the Asian monsoon and westerlies circulations. Copyright © 2016 John Wiley & Sons, Ltd. Article in Journal/Newspaper North Atlantic Wiley Online Library Pacific Hydrological Processes 30 13 2211 2222 |
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Wiley Online Library |
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crwiley |
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English |
description |
Abstract In this study, the regional tree‐ring chronology of Picea crassifolia was used to estimate annual (September to August) streamflow of the Shiyang River for the period from AD 1765 to 2010. The linear regression model was stable and could explain 41.5% of the variance for the calibration period of 1955–2005. According to the streamflow reconstruction, dry periods with below average streamflow occurred in AD 1775–1804, 1814–1823, 1831–1856, 1862–1867, 1877–1885, 1905–1910, 1926–1932, 1948–1951, 1960–1963 and 1989–2002. Periods of relatively wet years are identified for AD 1765–1774, 1805–1813, 1824–1830, 1857–1861, 1868–1876, 1886–1904, 1911–1925, 1933–1947, 1952–1959, 1964–1988 and 2003–2010. Comparisons with the precipitation reconstructions from surrounding areas supplied a high degree of confidence in our reconstruction. Our reconstructed streamflow is significantly correlated with sea surface temperature in the eastern equatorial Pacific Ocean and the North Atlantic Ocean. The Multitaper spectral and correlation analyses also suggested that the reconstructed streamflow variation in the Shiyang River could be associated with large‐scale atmospheric‐oceanic variability, such as El Niño‐Southern Oscillation (ENSO). The linkages among the streamflow reconstruction, NAO and ENSO suggest the connection of regional streamflow variations to the Asian monsoon and westerlies circulations. Copyright © 2016 John Wiley & Sons, Ltd. |
author2 |
National Basic Research Program of China Meteorology Public Welfare Industry Research Special Project Basic Research Operating Expenses of the Central-level Non-profit Research Institutes China Desert Meteorological Science Research Foundation |
format |
Article in Journal/Newspaper |
author |
Chen, Feng Yuan, Yu‐jiang Zhang, Rui‐bo Wang, Hui‐qin Shang, Hua‐ming Zhang, Tong‐wen Qin, Li Fan, Zi‐ang |
spellingShingle |
Chen, Feng Yuan, Yu‐jiang Zhang, Rui‐bo Wang, Hui‐qin Shang, Hua‐ming Zhang, Tong‐wen Qin, Li Fan, Zi‐ang Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent |
author_facet |
Chen, Feng Yuan, Yu‐jiang Zhang, Rui‐bo Wang, Hui‐qin Shang, Hua‐ming Zhang, Tong‐wen Qin, Li Fan, Zi‐ang |
author_sort |
Chen, Feng |
title |
Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent |
title_short |
Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent |
title_full |
Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent |
title_fullStr |
Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent |
title_full_unstemmed |
Shiyang River streamflow since AD 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude Asian continent |
title_sort |
shiyang river streamflow since ad 1765, reconstructed by tree rings, contains far‐reaching hydro‐climatic signals over and beyond the mid‐latitude asian continent |
publisher |
Wiley |
publishDate |
2016 |
url |
http://dx.doi.org/10.1002/hyp.10788 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10788 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10788 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Hydrological Processes volume 30, issue 13, page 2211-2222 ISSN 0885-6087 1099-1085 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/hyp.10788 |
container_title |
Hydrological Processes |
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30 |
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13 |
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2211 |
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2222 |
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1800757697889435648 |