In the tropical Northwest Pacific, DOM dynamics was jointly regulated by physical processes, phytoplankton production, photochemical reactions and microbial processes

In the tropical Northwest Pacific, organic matter fluorescence effectively traces frontal mixing processes

The quasi-permanent cold Mindanao and warm Halmahera eddy pair enhanced lateral dissolved organic matter transport in the western boundary current system

At Cape Hatteras, the nature of Gulf Stream position and transport variability changes over a 60-km distance from a red to a blue spectrum

Wave-like Gulf Stream meanders decay approaching Cape Hatteras with temporal amplitude variability that may be driven by the Loop Current

Florida Current transport maxima, coherent along the South Atlantic Bight, precede offshore Gulf Stream shifts downstream of Cape Hatteras

Dense waters overflowing the Iceland-Scotland ridge nearly double their volume transport through entrainment of lighter ambient waters

The export of the Iceland-Scotland Overflow Water from the Iceland Basin is approximately 5.3 Sv net of interior recirculation

The transport of the Iceland-Scotland Overflow plume found in this study is larger than most previously published estimates

An anomalous phytoplankton bloom occurred in the slope region under the influence of a mesoscale eddy and the Pearl River Plume

The nutrients supporting the bloom were not directly sourced from the Pearl River but were injected locally from subsurface

The interaction of freshwater from the Pearl River and eddy edge enhances frontal dynamics facilitating nutrient transport

Trophic structure of mesozooplankton is regulated by similar environmental factors such as phytoplankton assemblages

Diazotrophy and nutrient availability correlated with enhanced mesozooplankton carnivory in a complex tropical marine ecosystem

Mass and energy transfer across trophic levels of planktonic food webs are less efficient in spatially and temporally variable ecosystems

Dominant forcing mode and magnitude of net sand transport are predictable from readily available data using a k-Nearest Neighbor algorithm

Sand waves increase in length and asymmetry, and decrease in height, for increasing wave-dominance under extreme conditions

Over an average year, meso-macrotidal areas are tide-dominated, while shallow, finer grained, microtidal regions are wave-dominated

Both Chlorophyll-a (Chl) and particulate organic carbon (POC) in the Ross Sea are markedly underestimated using the NASA standard algorithms

Rrs667-based algorithms are locally tuned for the Ross Sea, with significantly improved performances in retrieving Chl and POC

The algal bloom signals in the Ross Sea are significantly higher than previously determined

A one-dimensional model is used to analyze 8 years of winter mooring data of the upper water column in a perennially ice-covered fjord

Mixing is more pronounced in the isolated freshwater layer (epishelf lake) than in the seawater below

Epishelf lake water exits the fjord through a basal channel under the ice shelf. The channel is apparently not evolving rapidly

Denitrification shifts nutrient stoichiometry and the phytoplankton community structure in the northern Benguela

Denitrification and anammox interact to limit growth of picophytoplankton, and favor a flagellate-dominated community structure and diatoms succession

The shift in nutrient stoichiometry and phytoplankton community structure from combined effects of denitrification and anammox result in a decrease in dissolved inorganic carbon uptake