also the gulf stream, involves the movement of layers of surface and deep water that distribute heat and control the climate
friction with prevailing winds on the ocean surface to the north east causes surface water to flow north east
water in north east atlantic sinks as it cools at the poles, drawing in warm water to replace it
higher atmospheric temperatures cause land ice in greenland to melt and flow into the sea, diluting the saline seawater to freshwater and causing it to sink beneath seawater, disrupting and slowing the rate
the sequence of naturally occuring events every 2-7 years and sees change in wind patterns which result in different precipitation patterns and current directions
trade winds travelling west from south america to indonesia change direction, travelling from indonesia to s. america
nutrient rich water from the deep ocean is drawn up along the coast of south america, causing large algal blooms that provide a food source for fisheries
wind direction changes, moves from indonesia to s. america, causes surface currents to change direction too
no upwelling to replace water drawn away by currents, no algal blooms due to nutrient deep water, so no food source for fish. fish die out and predators have no food, prey populations increase
there is no warm air carrying moisture rich air inland towards Australia and Asia
swapping of wind direction causes warm water to move eastward, which retain water vapour for longer and evaporation is increased
droughts in north east and south africa, and china
fewer hurricanes in north atlantic
fewer cyclones in japan
warmer atmosphere heats seawater which expands by 30%, causing the volume of the sea to increase and sea levels rise.
warming atmosphere causes ice to melt. land ice increases the volume as it is not already in the sea
no, it contracts when melting and occupies the same volume as ice below sea level
higher temperatures means the duration of ice and snow on the ground is shortened. snow and ice also melts quicker when its warmer
glaciers moving towards the sea due to effect of gravity may have the snout of the glacier melt faster than it is moving forward, causing the extent of the glacier to be reduced
meltwater from the top of a glacier may move to the bottom through cracks where it can lubricate the ice over the rock and allow it to move quicker. increasing temp means more meltwater and lubrication so quicker glacier
ice covering less than 50,000 km2 of land, thick enough to have its own topography
ice covering an area of over 50,000km2, these Greenland and Antarctica
decreasing due to higher temperatures, less ice means less albedo and less sun reflected, more ice melted, positive loop
during winters at the poles, ice sheets expand because of the low temps, with a warming climate this does not occur to the same extent, and is also relatively thin as it is ice that has crystallised in the sea
grounded ice sheets may float and break up earlier as sea levels rise as the ice breaks off earlier.
a large platform of glacial ice floating on the ocean