Four-Decade Coastal Evolution of Jiehe Beach in Northeastern Laizhou Bay: An Analysis Using Extensive Satellite Imagery
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摘要: 近几十年来,位于莱州湾东北部的界河两侧海滩(以下简称“界河海滩”)在河流入海泥沙减少背景下发生严重侵蚀,再加上裕龙岛(一个大型离岸人工岛)等沿海工程建设的影响,界河海滩的海岸线演变异常复杂。本文使用1984−2024年的
1186 幅卫星图像,采用聚焦剖面方法和亚像素海岸线识别技术研究界河海滩的海岸线演变,评估河流输沙和沿海工程的影响。结果显示界河海滩早期(1984−2004年)的演变主要受界河河口的封闭和打开、沙嘴的沿岸运移以及沙坝的向岸运移控制,总体上发生侵蚀;界河海滩后期(2004−2024年)的演变主要受裕龙岛等沿海工程建造影响,总体上发生淤进。在沿海开发日益加剧的今天,合理布局沿海工程有望减缓海滩侵蚀。Abstract: In recent decades, the beaches on both sides of the Jiehe River (hereinafter referred to as Jiehe Beach) in the northeastern part of Laizhou Bay have suffered severe erosion against the backdrop of reduced riverine sediment input to the sea. Additionally, the construction of coastal engineering projects such as Yulong Island (a large artificial offshore island) has made the evolution of the Jiehe Beach shoreline exceptionally complex. This paper utilizes 1,186 satellite images from 1984 to 2024, employing a transect-focused method and sub-pixel shoreline recognition technology to study the evolution of the Jiehe Beach shoreline and assess the impacts of river sediment discharge and coastal engineering. The results show that the early evolution (1984−2004) of Jiehe Beach was primarily controlled by the closure and opening of the Jiehe River estuary, the alongshore movement of sand spits, and the onshore movement of sandbars, with overall erosion occurring. The later evolution (2004−2024) of Jiehe Beach was mainly influenced by the construction of coastal engineering projects such as Yulong Island, with overall accretion occurring. In today's era of intensifying coastal development, the rational layout of coastal engineering is expected to mitigate beach erosion.-
Key words:
- Remote sensing /
- Shandong Peninsula /
- shoreline /
- estuary closure /
- artificial offshore island
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图 6 界河河口在2013-2016年的打开和封闭过程
(a)2013/06/08(河口封闭);(b)2013/08/11(河口打开);(c)2013/11/15(环形河口沙坝初步形成);(d)2014/03/07(环形河口沙坝形成);(e)2014/06/27(环形沙坝向岸运移);(f)2016/01/08(河口沙坝与周边岸线平齐)。
Fig. 6 Open and close process of Jiehe Estuary in 2013-2016.
(a) 2013/06/08 (closure of the estuary); (b) 2013/08/11 (opening of the estuary); (c) 2013/11/15 (initial formation of the circular estuary sandbar); (d) 2014/03/07 (formation of the circular estuary sandbar); (e) 2014/06/27 (transport of the circular sandbar towards the shore); (f) 2016/01/08 (alignment of the estuary sandbar with the surrounding shoreline).
图 7 剖面J12-J18附近沿岸沙坝在1984-1987年的向岸输运和并岸过程
(a)1984/04/21(近岸破碎波指示了两条水下沙坝的位置和形态);(b)1986/12/07(离岸较近的沙坝在潮位较低时出露,局部与海滩连接);(c)1987/01/24(沙坝向岸移动);(d)1987/11/24(沙坝并岸后的海岸线明显向海突出)。
Fig. 7 Onshore migration and merging process of the coastal sandbars near transect J12-J18 in 1984-1987.
(a) 1984/04/21 (nearshore breaking waves indicate the location and shape of two underwater sandbars); (b) 1986/12/07 (the sandbar near the shore is exposed when the tide level is low, and is partially connected to the beach); (c) 1987/01/24 (sandbar moving to shore); (d) 1987/11/24 (the shoreline after the sandbars were merged was obviously protruding to the sea).
图 8 剖面J15-J17附近的沿岸沙嘴在1990−1993年的形成和并岸过程
(a)1990/10/31(沙嘴未形成);(b)1992/02/07(沙嘴开始形成);(c)1993/01/08(沙嘴向西南方向运移);(d)1993/11/24(沙嘴前锋在J17剖面处并岸,在滩面形成微型潟湖)。
Fig. 8 Formation and merging process of the coastal spit near the transect J15-J17 in 1990-1993.
(a) 1990/10/31 (sand spits not formed); (b) 1992/02/07 (sand spits began to form); (c) 1993/01/08 (sand spits migration to the southwest); (d) 1993/11/24 (the front of sand spits merged at the J17 section and formed a micro-lagoon on the beach).
图 9 剖面J16-J19附近的沿岸沙嘴在1996-1999年的形成和并岸过程
(a)1996/05/08(沙嘴未形成);(b)1997/01/03(沙嘴开始形成);(c)1998/05/14(沙嘴向西南方向运移);(d)1999/12/27(沙嘴在J19剖面附近并岸)。
Fig. 9 Formation and merging process of the coastal spit near the transect J16-J19 in 1996-1999.
(a) 1996/05/08 (sand spits not formed); (b) 1997/01/03 (sand spits began to form); (c) 1998/05/14 (sand spits migration to the southwest); (d) 1999/12/27 (sand spits merged near the J19 section).
表 1 海岸线位置的随机误差(单位:m)
Tab. 1 Random error of satellite-derived shoreline position (unit: m)
剖面 未校正的海岸线
(水边线)地理校正后
的海岸线地理、潮位校正后的海岸线
(平均潮位线)J1 5.4 5.2 4.8 J2 5.4 5.0 4.7 J3 4.8 4.4 4.2 J4 5.0 4.8 4.5 J5 4.9 4.7 4.6 J6 4.8 4.6 4.4 J7 6.1 5.9 5.6 J8* 9.5 9.3 9.0 J9* 11.9 11.9 11.9 J10 5.7 5.4 5.1 J11 5.4 5.3 4.9 J12 6.3 6.1 5.8 J13 5.3 5.1 4.8 J14 5.2 5.0 4.7 J15 5.8 5.5 5.3 J16 5.4 5.3 5.2 J17 5.9 5.9 5.7 J18 5.3 5.2 5.1 J19 6.1 6.0 5.7 J20 5.9 5.7 5.3 J21 6.1 5.9 5.5 J22 5.8 5.7 5.3 J23 5.4 5.2 4.9 J24 7.0 6.7 6.2 J25 5.5 5.2 5.0 J26 5.0 4.8 4.6 平均 6.0 5.8 5.5 * J8和J9剖面的较大位置误差主要是界河河口沙坝的剧烈变化所致。 表 2 沿海工程建设前后邻近海滩的海岸线变化速率
Tab. 2 Shoreline change rates at the adjacent beaches of the coastal projects before and after their construction
剖面 沿海工程 建设时间 建设前海岸线变化速率 (m·a−1) 建设后海岸线变化速率 (m·a−1) 海岸线变化速率增量 (m·a−1) 影响时长 (a) J4 裕龙岛 2011 −1.0 7.9 8.9 3 J5 裕龙岛 2011 −3.0 15.1 18.1 6 J6 裕龙岛 2011 1.4 4.8 3.4 9 J16 丁坝1 2010 −5.6 22.1 27.7 2 J17 丁坝1 2010 −0.8 −1.6 −0.8 3 J18 丁坝1 2010 0.5 −19.0 −19.5 3 J20 丁坝2 2017 −3.1 3.1 6.2 6 J21 丁坝2 2017 −0.5 3.6 4.1 6 J22 丁坝2 2017 −1.7 −0.7 1.0 6 J23 丁坝3 2006 0.4 13.2 12.8 5 J24 丁坝3 2006 0.2 −8.7 −8.9 5 J24 春雨码头 2011 −8.7 28.7 37.4 4 J25 春雨码头 2011 0.2 7.4 7.2 4 -
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