Smaller, younger leaves may be better; a frost sometimes boosts the sweet side of Brassicas; or, soaking leaves
in warm salty water for half an hour before roasting might be helpful.
Many factors — like the thermohaline circulation, which reverses direction at the poles
as warm salty water releases heat into the air and sinks down to the bottom — are heavily influenced by the ocean's salinity, and thus, the movement of freshwater into and around the Arctic plays an important role in shaping both regional and global climate.
The decaying rings provide a source of
warm salty water important for the global thermohaline circulation (de Ruijter et al., 1999), and variations in that exchange may generate THC variations.
The Gulf Stream transports
warm salty water from the subtropical region to mid-latitudes in the North Atlantic, and changes in its path can have a strong impact on regional marine ecosystems and fisheries.
Rinse out your mouth
with warm salty water (sea salt), and follow up with a good brushing using toothpaste or whatever cleanser you prefer.
The «Agulhas leakage»
of warm salty waters from the Indian Ocean, appears to be increasing, says the study - and that could help prevent the predicted slow - down of the North Atlantic Drift.
Wash with
warm salty water or dilute hydrogen peroxide (50/50 10 volume).
One day, before heading out into
the warm salty water, he read to us a moving passage about the powerful effect of surfing on the human brain, from the recent book «Blue Mind», by well - known marine biologist and fervent ocean conservationist Wallace J. Nichols.
Temperatures in the Gulf of Maine are subject to extreme variability due to the interactions between colder, fresher water currents from the north and
warmer saltier water from the south as well as atmospheric fluctuations, according to UMaine researchers.
The authors postulated that
this warm salty water (WSW) layer, situated beneath the colder surface freshwater in the North Atlantic, generated ocean convective available potential energy (OCAPE) over decades at the end of HS1.
According to fluid modelling, at one point the accumulation of OCAPE was released abruptly (~ 1 month) into kinetic energy of thermobaric cabbeling convection (TCC), resulting in
the warmer salty waters getting to the surface and subsequently warming of ca. 2 °C sea surface warming.
But your link shows that
warm saltier water can be denser than colder fresher water, I should have remembered that as it is one of the factors that drives the thermo - haline circulation.
Furthermore, it will churn things up big time and bring up
warmer saltier water.