While previous studies focus on ensemble mean variability due to sea surface temperature forcing, this study examines atmospheric internal variability that
affects cyclone track distributions.
Not exact matches
An increase in the width of the tropics could increase the area
affected by tropical storms (hurricanes), or could change climatological tropical
cyclone development regions and
tracks.
Further complicating the use of these proxies is the fact that the deviation in oxygen - 18 ratios is
affected by the amount of TC rainfall, the distance from the center of the
cyclone at which the rain was produced, and the intensity of the
cyclone — so I doubt these proxies alone will enable disentangling intensity and rainfall, tnough a large number of samples over an area could reveal information about the
track and extent of the TC event.
Moderate to strong correlation between CanSIPS mean storm
track density and ERA - Interim
track density are found across the primary storm
track in the North Pacific and in the primary formation regions for Atlantic
cyclones affecting North America (Gulf of Mexico and Cape Hatteras) Most CanSIPS bias in the North Pacific is centralized in the exit regions of the Pacific storm
track, localized to Gulf of Alaska and coastal BC.