
Massive melting of land ice is also changing ocean chemistry
25%
The massive Greenland ice cap is shrinking an by average of 30 million tons an hour – which is 20% more than was previously thought. This additional source of freshwater pouring into the North Atlantic contributes to the slowing of the Atlantic meridional overturning circulation (AMOC), a dire state of affairs for Europe.
More on AMOC slowdown and other tipping points.
Ice loss from Antarctica continues to accelerate and is now estimated at 150 Gigatons per years. This is a sevenfold increase since the 80’s and adds an additional .5 mm per year to sea levels.
Globally, mountain glaciers have been losing mass rapidly and contribute around 0.2 to 0.4 mm per year to sea-level rise.
SURPRISE!
Groundwater depletion is rapidly moving water to oceans, and under the radar source of sea level rise
25%
THE THIRD CAUSE IS UNKNOWN TO MOST PEOPLE.
Groundwater depletion from irrigation and other human activities is a major though often overlooked, contributor to sea level rise, adding new freshwater to oceans that was previously stored on land. A relatively recent discover, this category of water transfer to the oceans may now equal or exceed melting glaciers and ice sheets. This human activity is causing a global shift in the water cycle, which is virtually never a good thing for humans.


Thermal expansion of the ocean contributes more to sea level rise than melting polar ice
50%
About half of current sea level rise is attributable to ocean thermal expansion. When seawater warms, it expands, and takes up more volume, significantly contributing to sea-level rise. as oceans absorb over 90% of Earth’s trapped heat from greenhouse gases, causing water molecules to spread out, leading to rising coastal waters. This process accounts for about half of global sea-level rise, with warmer temperatures increasing the total volume (not the amount of water, but rather the space the water takes up) of water in the planetary ocean, impacting coastal areas and ecosystems worldwide.

Greenland and the slowing AMOC
GREENLAND AND THE AMOC
The Atlantic Meridional Overturning Circulation (AMOC) is weakening, This slowdown, driven by Greenland ice melt and increased freshwater in the North Atlantic, threatens to cause severe weather shifts, including rapid European cooling, enhanced Atlantic sea-level rise, and intense drought.
When examined independently, the accelerating melt rate of the Greenland Ice Sheets and the slowing of the AMOC are alarming in a fairly obvious way. There are trillions of tons of fresh water ice atop the Greenland land mass. As it continues to melt at ever increasing rates, it will add to ocean volume and sea level rise. The AMOC (Atlantic Meridional Overturning Circulation), which includes the Gulf Stream, carries warm tropical water to the North Atlantic, which moderates the temperatures of Northern Europe. The slowing of this ocean stream will fundamentally alter the climate of Europe.
LESS HEAT MOVING NORTH TO WARM EUROPE
The relationship between these two systems is based on the fact that the AMOC is driven by water salinity. When the waters cool in the northern reaches, they sink to the bottom, which creates the overturning effect. That powers the current. When huge quantities of fresh water are dumped into the salt water ocean, the salinity changes and the power of the overturning system is diminished.
A weakened AMOC is also likely to compromise the northern Amazonia rain forest and bring warmer waters to Antarctica, hastening the coastal ice shelves collapse.


















































