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Other options. This disappearing ice is creating conditions that are more favourable for N. During the winter monsoon season in the Indian Ocean region, cold, dry winds blow from the plateau toward the ocean.
They cool the surface waters of the northern Arabian Sea as they sweep across it. Cooler water sinks and warmer nutrient-rich water from the seafloor replaces it, a process of convective mixing.
With diminished ice cover, the landmass is heating up more than usual, so winds blowing over the sea are warmer and less dry than before.
This has weakened the convective mixing and disrupted nutrient supply to the sea surface, the study authors say.
But then as stratification sets in, the ability to survive and thrive in low nutrients conditions advantages it further.
Nor are they convinced that the loss of ice on the Himalayan-Tibetan Plateau is behind the waning of the convective process.
According to Prakash, the disappearing diatoms could be explained by the low silicate levels in the water. Gomes said the absence of silica does not explain why other phytoplankton that do not require the mineral had not taken the place of diatoms.
What they agree on is that the green sea sparkle is flourishing in conditions hostile to other plankton. Blooms are found throughout temperate to sub-tropical regions, with significant concentrations off the coasts of Central America, the Turkish Straits, Southeast Asia, and Europe.
Gustaaf Hallegraeff, a professor of marine science at the University of Tasmania, studies red N. He said there was a clear climate change signal in the migration of the blooms southward from the Australian mainland toward Tasmania.
The possibility of the blooms drifting further into the Southern Ocean that surrounds Antarctica worries Hallegraeff. It could pose a similar threat to diatom blooms there.
He described the impact of N. Studies on the relationship between the yearly Arabian Sea outbreaks and fisheries, however, are scarce.
Prakash said N. There are reports of N. Gohil, a resident of Chimbai, said on a winter morning in , when I visited the settlement in the state of Maharashtra.
The fishers I spoke to in Chimbai agreed with the surveyed fishers that industrial fishing was a big reason for their withering fishing fortunes.
Coastal megacities in India generate more than 6 billion liters 1. Overall, the country can treat only about a third of its sewage. That means billions of liters of untreated sewage are being flushed into the Arabian Sea every year.
Its waters are naturally sluggish, preventing oxygen mixing. Sewage and agricultural runoff dumped in the sea soaks up oxygen as it decomposes, creating zones where marine species struggle to survive.
The outbreaks are expansive; in satellite imagery, they appear like spirals of oily green paint stretched across the entire northern Arabian Sea.
When the N. A more stratified water column, skewed nutrient availability and oxygen loss all point to profound changes in the Arabian Sea.
Scientists like Gomes and Goes see the sea sparkle blooms as not just a symptom of the changing environmental conditions, but as a trigger for disruptions yet to come.
Despite all the changes that Chimbai residents are witnessing, the sea remains a reassuring presence. No matter what humans throw at the sea, it remains unscathed.
That worldview could be upended at a time when human activities are transforming the seas in unprecedented ways.

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