The Indian Ocean is warming faster than any of the global oceans and its climate is uniquely
driven by the presence of a landmass at low latitudes, which causes monsoonal winds and …

Nitrogen and phosphorus concentrations in oceans have been extensively studied, and
advancements in associated disciplines have rapidly progressed, enabling the exploration …

Coastal ecosystems are amongst the most vulnerable to climate change, due to their
location at the land-sea interface. In coastal waters, the nitrogen cycle can be significantly …

Marine settings provide major carbon sinks for organic carbon, and act as a key reservoir
that can sequester excess carbon during times of high CO 2 and global warming. Organic …

Kuroshio intrusion (KI) is a key process that transports water from the western Pacific Ocean
to the northern South China Sea (nSCS), where KI-induced surface water mixing often …

Observations show a decreasing trend in sea surface salinity during the winter months in
1990–2010 in the southeastern Arabian Sea. To explain the observed salinity decline, we …

Nitrogen (N) and phosphorus (P) determine the strength of the ocean's biological carbon (C)
pump, and variation in the N: P ratio is key to phytoplankton growth. A fixed C: N: P ratio …

Saline lakes across the globe have experienced severe reduction in their surface area as a
result of climate change and human-induced perturbations like water diversion and …

As climate change progresses, the intensity and variability of freshwater outflow into the
ocean is predicted to increase. The resulting increase in low-salinity events will be a source …

Nitrogen (N 2) is an essential macronutrient and plays an essential role in maintaining
growth and yield of plants. This being the case, it is imperative to recognize the key traits …