声明 发表于 2025-3-30 09:42:29
http://reply.papertrans.cn/83/8229/822857/822857_51.pngIOTA 发表于 2025-3-30 15:11:22
Nurhan Çolakogluh-resolution depth-averaged numerical model computed the tidal circulation driven by the principal lunar semi-diurnal constituent M.. The initial particle positions were taken at the 14,026 nodes of the unstructured computational grid surrounding the area of interest with a spatial resolution belowImplicit 发表于 2025-3-30 16:42:22
http://reply.papertrans.cn/83/8229/822857/822857_53.pngEssential 发表于 2025-3-30 23:16:33
Stephan Ramon Garciaeatened by salt water. The salinity would be greatly reduced in the water sources intake with the North Branch blocked. The salinity of the water intake in the Dongfengxisha Reservoir and Chenhang Reservoir would be close to 0 in any condition while the Qingcaosha Reservoir is still threatened by sa极为愤怒 发表于 2025-3-31 01:41:34
http://reply.papertrans.cn/83/8229/822857/822857_55.png闪光东本 发表于 2025-3-31 07:42:39
Sawinder P. Kaur,Israel Koltracht 25–50 percent of that produced) is associated with a large flux of inorganic nutrients from the sediments to the overlying water. The stoichiometry of net benthic nutrient regeneration differs from that of pelagic regeneration, however, and simple Redfield type models probably cannot be applied. Th柏树 发表于 2025-3-31 11:01:22
http://reply.papertrans.cn/83/8229/822857/822857_57.png乏味 发表于 2025-3-31 13:56:59
http://reply.papertrans.cn/83/8229/822857/822857_58.png不透明性 发表于 2025-3-31 20:35:50
Leiba Rodman,Ilya M. SpitkovskyTM zones was modulated by spring and neap tidal conditions. From our simulations we demonstrated that the sediment transport of small particles, e.g. 2 μm particle size, in DH is driven by flood dominance, which is affected by wet/dry areas such as mangroves and tidal flats. Therefore, mangrove area气候 发表于 2025-3-31 23:29:33
James Rovnyak,Lev A. Sakhnovich non-flood conditions) as well as the ability of the system to adapt to long term changes (i.e. past morphological and ecosystem shifts) suggests that Moreton Bay and its associated estuaries have significant capacity to adapt to change. Whether the current rate of anthropogenically induced change i