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使用水动力模型的岛屿与大陆之间的高程系统连接:以连接荷兰瓦登群岛与阿姆斯特丹 Ordnance 基准面(NAP)为例

Height system connection between island and mainland using a hydrodynamic model: a case study connecting the Dutch Wadden islands to the Amsterdam ordnance datum (NAP).

作者信息

Slobbe D C, Klees R, Verlaan M, Zijl F, Alberts B, Farahani H H

机构信息

1Delft University of Technology, Stevinweg 1, 2628 CN Delft, The Netherlands.

2Deltares, Boussinesqweg 1, 2629 HV Delft, The Netherlands.

出版信息

J Geod. 2018;92(12):1439-1456. doi: 10.1007/s00190-018-1133-3. Epub 2018 Mar 9.

DOI:10.1007/s00190-018-1133-3
PMID:30930554
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6405183/
Abstract

We present an efficient and flexible alternative method to connect islands and offshore tide gauges with the height system on land. The method uses a regional, high-resolution hydrodynamic model that provides total water levels. From the model, we obtain the differences in mean water level (MWL) between tide gauges at the mainland and at the islands or offshore platforms. Adding them to the MWL relative to the national height system at the mainland's tide gauges realizes a connection of the island and offshore platforms with the height system on the mainland. Numerical results are presented for the connection of the Dutch Wadden islands with the national height system (Normaal Amsterdams Peil, NAP). Several choices of the period over which the MWLs are computed are tested and validated. The best results were obtained when we computed the MWL only over the summer months of our 19-year simulation period. Based on this strategy, the percentage of connections for which the absolute differences between the observation- and model-derived MWL differences are  cm is about 34% (46 out of 135 possible leveling connections). In this case, for each Wadden island we can find several connections that allow the transfer of NAP with (sub-)centimeter accuracy.

摘要

我们提出了一种高效且灵活的替代方法,用于将岛屿和近海潮汐测量站与陆地高度系统相连接。该方法使用一个区域高分辨率水动力模型来提供总水位。通过该模型,我们获取了大陆上潮汐测量站与岛屿或近海平台之间平均水位(MWL)的差异。将这些差异加到相对于大陆潮汐测量站国家高度系统的平均水位上,实现了岛屿和近海平台与大陆高度系统的连接。给出了荷兰瓦登群岛与国家高度系统(阿姆斯特丹正常水位,NAP)连接的数值结果。对计算平均水位所采用的时间段的几种选择进行了测试和验证。当我们仅在19年模拟期的夏季月份计算平均水位时,获得了最佳结果。基于此策略,观测得出的平均水位差异与模型得出的平均水位差异之间绝对差值在 厘米以内的连接比例约为34%(135种可能的水准测量连接中有46种)。在这种情况下,对于每个瓦登岛,我们都能找到几种连接方式,可实现以(亚)厘米精度传递NAP。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/15d4c14551c0/190_2018_1133_Fig17_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/15d4c14551c0/190_2018_1133_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/2092d5698e97/190_2018_1133_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/d3037ffc81c2/190_2018_1133_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/ee05cdf8c532/190_2018_1133_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/ed84ed81a051/190_2018_1133_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/3338069597b1/190_2018_1133_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/f9be67d4eb2d/190_2018_1133_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/ef3c0ebbf3eb/190_2018_1133_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/827d893320a6/190_2018_1133_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/b217e688bd20/190_2018_1133_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/6039abc8d9c0/190_2018_1133_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/0837c20e7368/190_2018_1133_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/601b67939539/190_2018_1133_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/a02c34e36498/190_2018_1133_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/a1a44c75acc1/190_2018_1133_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/a618926be24e/190_2018_1133_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/d4f9512775db/190_2018_1133_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e78b/6405183/15d4c14551c0/190_2018_1133_Fig17_HTML.jpg

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