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In New Zealand, there is forecast to be stronger winds and more high intensity rainfall as well as less risk of fungal disease in drier areas but increased risk from fire and insect attack.
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I D and I MAP D thresholds for landslides and debris flows show that debris flows tend to occur during more severe (high intensity) rainfall conditions than landslides.
We found that the diurnal pattern is more prominent for the high intensity rainfall than that for the low rainfall intensity.
In terms of impact of increased rainfall and storms on sediment output, the more frequent returns of high intensity rainfall increases sediment output but average concentration may reduce as a result of the increased discharge.
However, later studies of high intensity rainfall in countries around the world established more realistic values for the energy of high intensity rainfall and these have now been incorporated into the USLE.
Infrequent, high intensity rainfall or snowmelt causes a particularly high flood risk to these karst areas.
The climate in the central highlands is sub-humid to semi-arid subtropical, and rainfall is highly variable, strongly summer-dominant with common summer high intensity rainfall events.
Climate change is predicted to lead to an increased frequency of high intensity rainfall events.
At both scales, high intensity rainfall above a threshold was responsible for inducing most of the geomorphic change.
The Hawke's Bay region experiences a variable climate with summer droughts and high intensity rainfall events (Thompson [1987]).
Observations of high intensity rainfalls have been recorded at gauging stations in many parts of the world.
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