6) There is less eK in the entire A during ice ages, and
cold ocean waters also store (sink) more CO2 within.
Not exact matches
And around Antarctica, where even the surface
ocean water is already quite
cold and dense, some of that
water in the
ocean depths, which is
also carbon rich, eventually warmed enough so that it became less dense than the
water above it.
«The
water in the Arctic and Antarctic
Oceans is extremely
cold, but
also very rich in oxygen.
For example, the Antarctic icefish, a pale, near - transparent inhabitant of the frigid South Atlantic
Ocean, has not only lost its ancestors» power to make oxygen - binding red hemoglobin (which it does not need in the
cold oxygen - rich
waters) but the two genes that code for hemoglobin have
also gone extinct: one has disappeared, and the other remains as a non-coding «molecular fossil,» a useless remnant that hints at past use but still resides in the icefish DNA.
Diving right in Ray, who was one of the first scientists to use scuba diving to study marine animals in polar environments, has not only observed the biological adaptations that mammals employ in
cold ocean waters, but has
also experienced prolonged immersion in those
waters firsthand.
Ray, who was one of the first scientists to use scuba diving to study marine animals in polar environments, has not only observed the biological adaptations that mammals employ in
cold ocean waters, but has
also experienced prolonged immersion in those
waters firsthand.
My research indicates that the Siberian peat moss, Arctic tundra, and methal hydrates (frozen methane at the bottom of the
ocean) all have an excellent chance of melting and releasing their stored co2.Recent methane concentration figures
also hit the news last week, and methane has increased after a long time being steady.The forests of north america are drying out and are very susceptible to massive insect infestations and wildfires, and the massive die offs - 25 % of total forests, have begun.And, the most recent stories on the Amazon forecast that with the change in rainfall patterns one third of the Amazon will dry and turn to grassland, thereby creating a domino cascade effect for the rest of the Amazon.With co2 levels risng faster now that the
oceans have reached carrying capacity, the
oceans having become
also more acidic, and the looming threat of a North Atlanic current shutdown (note the recent terrible news on salinity upwelling levels off Greenland,) and the change in
cold water upwellings, leading to far less biomass for the fish to feed upon, all lead to the conclusion we may not have to worry about NASA completing its inventory of near earth objects greater than 140 meters across by 2026 (Recent Benjamin Dean astronomy lecture here in San Francisco).
There is
also a contribution of excess atmospheric CO2 absorption introduced to deep -
water masses from dense,
cold CO2 - rich surface
waters at downwelling sites (e.g., North Atlantic), which then move through the
oceans via meridional overturning circulation.
If this is the case, we might
also find Europan planets with an abundance of subsurface oxygenated
water, which could bubble out to form habitable caves in the ice above a
cold ocean.
Omega - 3 fats are found mostly in
cold -
water ocean fish, and
also in beans, flaxseed, walnuts, vegetables, and in wild and grass - fed animals (although in much lower quantities).
Puri Wirata Amed - Dive Resort and Spa is a budget PADI five - star resort located in Bunutan, a quiet fishing village along the coast of Amed, a premier diving destination in East Bali.The resort is a two - hour transfer from the Ngurah Rai International Airport in South Bali, and an hour from the breach resort area of Candidasa.Puri Wirata Amed offers a collection of
ocean - view guestrooms and villas equipped with air conditioning, hot and
cold water, balcony or terrace, four - poster beds with mosquito nets, personal safe, mini-bar, flat screen television and DVD players.Two
ocean front swimming pools and direct beach access make for a memorable outdoors for guests staying at Puri Wirata, and an onsite restaurant that serves a variety of Indonesian, Balinese and Western dishes
also makes for an ideal spot from where to enjoy the views with a cocktail at hand.
Body suits have become popular in recent years and are
also rented so that guests do not get too
cold in the Pacific
Ocean waters.
Ray Ladbury wrote at 27 «However, there is
also a huge reservoir of
cold water in the deep
oceans.
However, there is
also a huge reservoir of
cold water in the deep
oceans.
The study
also found that the movements of all of the
ocean's marine life — from lowly phytoplankton to the largest whales — play a crucial role in bringing
cold water from the
ocean's depths to the surface.
Scientists
also know that
ocean temperatures are rising because warm -
water species are moving into areas that were formerly too
cold, while cool -
water and
cold -
water species are likewise on the move.
AGW climate scientists seem to ignore that while the earth's surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take
water vapor scavenged from the vast
oceans on earth (which are
also a formidable heat sink), lift it to
cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts of heat from the atmosphere) or freeze it, (removing even more vast amounts of heat from the atmosphere) drop it on land and
oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the
oceans and building polar ice caps and even more importantly, increasing the albedo of the earth, with a critical negative feedback determining how much of the sun's energy is reflected back into space, changing the moment of inertia of the earth by removing
water mass from equatorial latitudes and transporting this
water vapor mass to the poles, reducing the earth's spin axis moment of inertia and speeding up its spin rate, etc..
LIA wasn't GLOBAL cooling; but
colder in Europe, north America — because Arctic
ocean had less ice cover - > was releasing more heat / was accumulating - > radiating + spreading more coldness — currents were taking that extra coldness to Mexican gulf — then to the Mediterranean — because Sahara was increasing creation of dry heat and evaporating extra
water in the Mediterranean — to top up the deficit — gulf stream was faster / that was melting more ice on arctic
also as chain reaction — Because Mediterranean doesn't have enough tributaries, to compensate for the evaporation deficit.
For example, reductions in seasonal sea ice cover and higher surface temperatures may open up new habitat in polar regions for some important fish species, such as cod, herring, and pollock.128 However, continued presence of
cold bottom -
water temperatures on the Alaskan continental shelf could limit northward migration into the northern Bering Sea and Chukchi Sea off northwestern Alaska.129, 130 In addition, warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If
ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are
also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.134
We
also have more brine rejection from sea ice that sends a lot of very
cold, very salty
water to the bottom of the
ocean in a hurry.
However, the upwelling of
cold water off of the east coast of South American is
also part of the meridional overturning of the
ocean that begins with the sinking of
cold salty
water near the poles (thermohaline circulation) that forms the characteristic deep
water found at the bottom of the major
oceans.
There is
also an increased upwelling of deep
cold ocean waters and more intense uprising of surface air near South America, resulting in increasing numbers of drought occurrences, although fishermen reap benefits from the more nutrient - filled eastern Pacific
waters.
As the temperature increased in the past,
oceans also released more carbon dioxide because warm
water holds less carbon dioxide than
cold water.
Ice formation expels most of its salts and makes the
also cold waters heavier than the deep
ocean waters.
It is
also often called an «overturning» circulation because
cold, salty
waters sink in the North Atlantic and travel back southward at deep
ocean depths.