Not exact matches
Dr Martin Ziegler, Cardiff University School of Earth and
Ocean Sciences, said: «We found that
South Africa experienced rapid climate transitions toward wetter conditions at times when the Northern
Hemisphere experienced extremely cold conditions.»
The Arctic took another 3,000 - 4,000 years to warm this much, primarily because of the fact that the Northern
Hemisphere had huge ice sheets to buffer warming, and the fact that changes in
ocean currents and Earth's orbital configuration accelerated warming in the
south.
The study, co-authored by Dr Thomas Stevens, from the Department of Geography at Royal Holloway, University of London, found a previously unknown mechanism by which the joining of North and
South America changed the salinity of the Pacific
Ocean and caused major ice sheet growth across the Northern
Hemisphere.
The Southern
Hemisphere, which includes the southern Indian
Ocean from the coast of Mozambique across Madagascar to the coast of Australia, into the
South Pacific and Coral Sea, saw below normal activity as well in 2008.
And meanwhile down
south exactly the same thing happened as in the far north, although [due to the reversed situation of a central continent and surrounding seas — instead of a central
ocean, surrounded by land masses] with exactly the opposite effect: the Antarctic sea ice reached its highest ever extent during the Southern
Hemisphere winter.
The northern
hemisphere has warmed faster than the southern because there's more land in the north than the
south, and land has far less thermal inertia than
ocean.
While these three types of measurements together suggest that our estimates of northern
hemisphere ocean warming are about right, a different story emerged for down
south.
Two reasons why this should be so in the real world are that, first, the Southern
Hemisphere subtropical gyres are situated mostly in the Southern
Ocean and
South Atlantic, and second, that some of the heat coming into the Pacific
Ocean basin doesn't actually stay there.
By comparing the
hemispheres to the tropical temperatures, you can see the shift of heat content from neutral, to north or
south and the different amplification due to the land /
ocean ratio of the
hemispheres.
It was predominantly warmer than average over the extratropical
oceans of the southern
hemisphere and over the North Pacific, but colder than average to the
south - west of South Ame
south - west of
South Ame
South America.
A new Indonesian coral - based record of surface
ocean salinity shows that the location of the most significant hydroclimatic feature in the Southern Hemisphere, the South Pacific Convergence Zone (SPCZ), a band of high clouds and precipitation, influences a major current in the far western Pacific O
ocean salinity shows that the location of the most significant hydroclimatic feature in the Southern
Hemisphere, the
South Pacific Convergence Zone (SPCZ), a band of high clouds and precipitation, influences a major current in the far western Pacific
OceanOcean.
Isaac Held considered north vs
south hemispheres which is really an imbalance of
ocean vs land temperatures.
Webster, «Isaac Held considered north vs
south hemispheres which is really an imbalance of
ocean vs land temperatures.»
With the approach of winter, temperatures in Northern
Hemisphere begin to cool more rapidly — and the region of maximum north -
south temperature differential over the Pacific
Ocean starts to shift southward.
The more recent suggestion is that it is triggered by changes in polar surface pressure which modulate wind and
ocean currents in both the north and
south hemispheres.
The southern
hemisphere tropical cyclone season normally runs from November to April and so far this season activity in the
South Pacific
Ocean has been relatively low.
This disrupted the warm
ocean flow of water from the Southern
hemisphere to the Northern Hemisphere, which caused the North to cool and the South t
hemisphere to the Northern
Hemisphere, which caused the North to cool and the South t
Hemisphere, which caused the North to cool and the
South to warm up.
Once North and
South American continents walled off eastern from western
hemispheres, global atmospheric -
ocean circulation patterns apparently lent themselves to regularly recurring chill phases.
Presenting their work at a recent European Science Foundation (ESF) conference, a group of scientists predicted that the saltiness of the waters of the southern
hemisphere oceans around
South Africa and New Zealand could serve as an early indicator of
«Skinner at all then argue that the
oceans transmitted the signal from the warming North (Milancovitch) to the
South (by shutting down the Meridional Overturning Circulation (MOC)-- heat remains in the Southern
Hemisphere, which would melt sea - ice, which leads to more mixing / upwelling of the deep
ocean as the
ocean is not «protected» by sea - ice anymore).
Part of the explanation is probably due to the fact that temperatures are more stable in the Southern
hemisphere (since land heats and cools faster than
ocean, and there is much more
ocean in the southern half of the globe), but the surface temperature records do not show such a north -
south differential.
Subarctic Climate Occurs mainly in Northern
hemisphere south of Arctic Ocean Winters are long and bitterly cold; summers short and cool Below freezing half the year Tundra Climate Coastal areas along the Arctic Ocean Long, bitterly cold winters In some parts is permafrost, or permanently frozen layers of soil Ice Cap Climate North and South poles Temperature lows of more than - 120 F Snow and ice remain year - round, but little precipitation Highland Climate Found on mountains Includes polar climates plus others; several climates in one As you go up a mountain, temperatures drop and plant life grows spa
south of Arctic
Ocean Winters are long and bitterly cold; summers short and cool Below freezing half the year Tundra Climate Coastal areas along the Arctic
Ocean Long, bitterly cold winters In some parts is permafrost, or permanently frozen layers of soil Ice Cap Climate North and
South poles Temperature lows of more than - 120 F Snow and ice remain year - round, but little precipitation Highland Climate Found on mountains Includes polar climates plus others; several climates in one As you go up a mountain, temperatures drop and plant life grows spa
South poles Temperature lows of more than - 120 F Snow and ice remain year - round, but little precipitation Highland Climate Found on mountains Includes polar climates plus others; several climates in one As you go up a mountain, temperatures drop and plant life grows sparser.
Cloud amount and albedo decreased over mid-latitude
oceans in both
hemispheres (especially over the North Atlantic), over the southeast Indian
Ocean, and in a northwest - to - southeast line stretching across the central tropical
South Pacific.»
In this paper the output from several different runs of a global
ocean GCM is used to show that the inflow of upper kilometer water in the
South Atlantic and the outflow of deep water varies in direct proportion to the westerly wind stress in the circumpolar region of the southern
hemisphere.