Zhou F., Ge J., Liu D., Ding P. A Lagrangian-based floating macroalgal growth and drift model (FMGDM v1. The model reference coordinate system is Cartesian and the tide station is spherical. Temporal and spatial distribution of red tide outbreaks in the Yangtze river estuary and adjacent waters, China. Northwestern Atlantic Ocean Text.
Provincetown to Nantucket - Text. Buzzards Bay - Text. Owing to the northwest wind-driven current and runoff, in the process of particles drift-diffusion in the sea area near Shenzhen Airport, the particles moved southward. Qin R., Lin L., Kuang C., Su T., Mao X. Little river weather sc. 1007/s12040-022-01811-6. 2022) used the high spatial resolution broad band optical satellite data from Chinese satellites GF-1 Wide Field of View (WFV), Haiyang 1D (HY-1D) Coastal Zone Imager (CZI), Sentinel-2 Multi-Spectral Instrument (MSI) and Landsat 8 Operational Land Imager (OLI) to detect fine-scale red tide. The length from the estuary to the open shelf is about 60 km and the width is 10-60 km. Received: 12 November 2022; Accepted: 27 January 2023; Published: 09 February 2023.
The drivers influencing the red tide drift-diffusion were analyzed through multiple control variable experiments. Li Y., Stumpf R. P., Mcgillicuddy D. J., He R. (2020b). 4 Guangdong Engineering Technology Research Center for Ocean Remote Sensing and Information Technology, Zhanjiang, China. Little River, SC Marine Weather Forecast. Hudson Canyon to Baltimore Canyon to 1000 Fathoms - Text. Compared with the no tide situation, it can be seen that under the influence of current, particles were distributed in a large area in the middle and south of Lingdingyang Bay (positive value) (Figure 8A). It is essential to pay more attention to red tide disasters and develop adequate red tide monitoring technologies for the Guangdong-Hong Kong-Macao Great Bay Area construction.
The model can well reproduce the development process of the red tide in the PRE, and can make up for the shortage of remote sensing data and measured data. 2 College of Chemistry and Environment, Guangdong Ocean University, Zhanjiang, China. Independent of geographical location and artificial conditions, satellite remote sensing has been widely used to analyze the temporal and spatial distribution of red tides. Based on the remote sensing image of red tide, Zhao and Ghedira (2014) used the results of the Hybrid Coordinate Ocean Model (HYCOM) and retrieval of sea surface temperature data from remote sensing to prove that the Arabian gulf red tide broke out offshore in 2008-2009 and was transported to the nearshore through the bottom Ekman layer advection. Doyle's family confirmed the wallet, which contained his SC ID, and the waders belonged to the missing hunter. Figure 7 Particles cloud distribution results on (A) October 26, 04:00; (B) October 26, 14:00; (C) October 26, 21:00; (D) November 1, 11:00; (E) November 1, 16:00; and (F) November 1, 23:00. Cape Charles Light to VA/NC Border - Text. Little river sc marine forecast office. All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. 4233/uuid:068a1257-dfc2-4389-964e-f665aa5cb213. The red tide started when Lingdingyang Bay was in a flood tide stage. Penobscot Bay - Text.
Marta Rodrigues, National Laboratory for Civil Engineering, Portugal. Without tidal current, the particles moved northward and concentrated in the sea area north of Neilingding Island. Our research also show that the red tide keeps aggregating along the coast under the influence of the northeast wind. Qu D., Yu H., Sun Y., Zhao Y., Wei Q., Yu H., et al. Liu L., Zhou J., Zheng B., Cai K., Tang J. The bathymetry data is obtained from ETOPO1. The astronomical tidal component is used as the outer sea boundary condition rather than the measured water level, which is conducive to the use of prediction simulation, but the accuracy of simulation in the past period will be reduced (Deltares, 2008). Little river sc marine forecast channel. Software 92, 252–260. Figure 8 The relative differences in the particles cloud distribution between the experiments. Therefore, this red tide had little impact on the upstream area. Manasquan Inlet to Little Egg Inlet - Text. Only the hydrodynamic process was considered in the model, without the red tide-related ecological process involved. Cape Charles to Currituck Beach 100 NM - Text.
Tracking migration and diffusion of red tides in qinhuangdao coastal water based on FBM method. As shown in Figure 4, the simulation results accurately reproduce the tide level variation of the PRE. Effects of physical and biochemical processes on the dissolved oxygen budget for the pearl river estuary during summer. We use the HY-1C/HY-1D Rayleigh-corrected products to identify the red tide.
Ding R., Chen X., Qu N. (2015). Li J., Xing Q., Zheng X., Li L., Wang L. 42 (9), 2969–2974. The river discharge boundaries include the estuaries at Humen, Jiaomen, Hongqili, and Hengmen. Both times the red tide impact areas were smaller compared to the previous five years.
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