Abstract—Tidal ocean corrections for gravity observation play an important part in monitoring studies. Tidal ocean models were tested by Transcontinental Tidal Gravity Profile (TTGP) results. This part of the global tidal network was used for study the influence of the Atlantic and Pacific oceans up to coastline. Our tidal result agrees with static theory and had a weak ocean dynamic influence (Schiwiderski and other models) into the center of the Eurasian continent. Near the coast, where ocean effects were strong, the influence increases. In the East part of TTGP, we obtained observation results for Khabarovsk region, for Sakhalin Island and for Primorye region (Sea of Okhotsk and Sea of Japan). In the South part of the Primorye observation (Russian Far East) long-term measurement was completed at the Posyet Bay level station and Cape Shultz gravity station. Based on the results, a selection of ocean tidal models was made and a number of unresolved issues were determined.

中文翻译：

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海洋潮汐模型和潮汐重力观测

摘要-用于重力观测的潮汐海洋校正在监测研究中起着重要作用。通过跨大陆潮汐重力剖面（TTGP）结果测试了潮汐海洋模型。全球潮汐网络的这一部分用于研究大西洋和太平洋对海岸线的影响。我们的潮汐结果符合静态理论，并且对欧亚大陆中心的海洋动力影响不大（Schiwiderski等模型）。在海洋影响强烈的海岸附近，影响增加。在TTGP的东部，我们获得了哈巴罗夫斯克地区，萨哈林岛和滨海边疆区（鄂霍次克海和日本海）的观测结果。在滨海边疆区的南部观测（俄罗斯远东地区），在Posyet湾水平站和Shultz角重力站完成了长期测量。根据结果​​，选择了海洋潮汐模型，并确定了许多未解决的问题。