Carrasco, J.F., D.H. Bromwich, and Z. Liu, 1997: Mesoscale
cyclone activity over Antarctica during 1991, Part 1: Marie Byrd Land.
Not exact matches
The greening of Sahara strengthens the West African Monsoon, which triggers a change in the atmospheric circulation
over the entire tropics, affecting tropical
cyclone activity.
Tracking changes in Arctic
cyclone activity through time, Vavrus calculated a statistically significant, though minor, increase in extreme Arctic
cyclone frequency
over the study period, with increases strongest near the Aleutian Islands and Iceland.
The article, «Extreme rainfall
activity in the Australian tropics reflects changes in the El Niño / Southern Oscillation
over the last two millennia,» presents a precisely dated stalagmite record of cave flooding events that are tied to tropical
cyclones, which include storms such as hurricanes and typhoons.
A tropical
cyclone is the generic term for a non-frontal synoptic scale low - pressure system
over tropical or sub-tropical waters with organized convection (i.e. thunderstorm
activity) and definite cyclonic surface wind circulation (Holland 1993).
Part of the difficulty in identifying the human component, if any is, as the IPCC Summary itself notes, that tropical
cyclone activity varies naturally
over the decades.
When we examine the relationship between SST and intensity, we find that although SSTs contribute significantly to tropical
cyclone activity, their influence varies markedly
over time.
Adam G: You can not conclude that just from looking at a basin which has less than 15 % of the total global tropical
cyclone activity, and also selecting groups of years that coincide exactly with the positive and negative Atlantic Multi-decadal Oscillation phases, which would dominate
over any AGW trend in this basin if it exists.
«Consequently, tropical
cyclone activity across the western Caribbean may remain essentially stable
over the current century, which has important implications for water availability in this region.
They found that averaged sea surface temperatures
over the MDR are the best predictor of Atlantic
cyclone activity, followed by global average surface temperature, with MDR warming relative to the tropics being the worst predictor of hurricane
activity (Figure 1).
A tropical
cyclone is a low pressure system
over tropical or sub-tropical waters, with convection (i.e. thunderstorm
activity) and winds at low levels, circulating either anti-clockwise (in the northern hemisphere) or clockwise (in the southern hemisphere).
In contrast to strong sea surface temperature control on basin counts, unpredictable internal variability in track density is strong
over the Gulf Coast and US East Coast - indicating that prediction of regional
cyclone activity, especially landfall hurricanes, is challenging.