Water level change of Lake Machang in eastern China over 1814–1902 CE

<p>Lake Machang, occupying an area of approximately 30 km<span class="inline-formula"><sup>2</sup></span> in the city of Jining, eastern China, was a historical reservoir on the Grand Canal from the early 15th century to early 20th century. The premodern month...

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Main Author: J. Fei
Format: Article
Language:English
Published: Copernicus Publications 2022-04-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/18/649/2022/cp-18-649-2022.pdf
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author J. Fei
author_facet J. Fei
author_sort J. Fei
collection DOAJ
description <p>Lake Machang, occupying an area of approximately 30 km<span class="inline-formula"><sup>2</sup></span> in the city of Jining, eastern China, was a historical reservoir on the Grand Canal from the early 15th century to early 20th century. The premodern monthly water level observation of Lake Machang commenced in 1814 CE and ended in 1902 CE. The available observation data from the monthly records covered 75.6 % of the entire study period of 1814–1902. Although the water level was seemingly artificially influenced by human activities, monthly and annual water level changes still correlated well with precipitation. That is, climate is still the dominant factor in water level changes on seasonal and annual scales. The flooding of the Yellow River in 1871 carried a large amount of silt into Lake Machang, which resulted in the rise of the lake bed and reclamation initiated by local residents. After the reclamation activity was officially approved in 1900, Lake Machang was massively reclaimed and eventually dried up in the early 20th century.</p>
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spelling doaj.art-b0fe2b90a91c4389a83a42b4686faacb2022-12-21T23:55:23ZengCopernicus PublicationsClimate of the Past1814-93241814-93322022-04-011864965510.5194/cp-18-649-2022Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CEJ. Fei<p>Lake Machang, occupying an area of approximately 30 km<span class="inline-formula"><sup>2</sup></span> in the city of Jining, eastern China, was a historical reservoir on the Grand Canal from the early 15th century to early 20th century. The premodern monthly water level observation of Lake Machang commenced in 1814 CE and ended in 1902 CE. The available observation data from the monthly records covered 75.6 % of the entire study period of 1814–1902. Although the water level was seemingly artificially influenced by human activities, monthly and annual water level changes still correlated well with precipitation. That is, climate is still the dominant factor in water level changes on seasonal and annual scales. The flooding of the Yellow River in 1871 carried a large amount of silt into Lake Machang, which resulted in the rise of the lake bed and reclamation initiated by local residents. After the reclamation activity was officially approved in 1900, Lake Machang was massively reclaimed and eventually dried up in the early 20th century.</p>https://cp.copernicus.org/articles/18/649/2022/cp-18-649-2022.pdf
spellingShingle J. Fei
Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CE
Climate of the Past
title Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CE
title_full Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CE
title_fullStr Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CE
title_full_unstemmed Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CE
title_short Water level change of Lake Machang in eastern China over 1814–1902&thinsp;CE
title_sort water level change of lake machang in eastern china over 1814 1902 thinsp ce
url https://cp.copernicus.org/articles/18/649/2022/cp-18-649-2022.pdf
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