Not exact matches
When an extreme event collides with continually rising seas, it takes a less
intense storm,
such as a Category I hurricane, to inflict as much coastal damage as a Category II or III
storm would have had when the seas were lower.
What he found was that not only were the simulations much closer to actual observations, but the high - resolution models were far better at reproducing
intense storms,
such as hurricanes and cyclones.
Extreme climate and weather events
such as record high temperatures,
intense downpours and severe
storm surges are becoming more common in many parts of the world.
Such relatively quiet seasons will likely continue to occur in the future thanks to the natural variations in Earth's climate, but the most
intense typhoons are likely to make up a higher percentage of the
storms that occur in the future.
What he found was that not only were the simulations much closer to actual observations, but the high - resolution models were far better at reproducing
intense storms,
such as hurricanes and cyclones.
Some of the effects of climate change are likely to include more variable weather, heat waves, heavy precipitation events, flooding, droughts, more
intense storms such as hurricanes, sea level rise, and air pollution.
Projections suggest an increase in extreme weather events,
such as heavy rainfall, more
intense storms and heat - waves.
The report states that with SIDS being completely dependent on ports and airports, climate change risks
such as rising sea levels, increasing temperatures and more frequent and / or
intense storms pose serious threats to vital transport infrastructure, services and operations.
As warming climate causes sea level rise, coastal urban areas
such as New York City face more frequent and
intense episodic flooding following
storms and inundation of some low - lying areas (2011-04-26) + Read Science Brief
Assuming a good bit of this was added after the natural warming cycle was started we are probably looking at closer to 1200 ppm over the next century or two before C02 levels begin to decrease again as this natural green house locks up carbon primarily in phytoplankton blooms caused by fertilization from the new large desert regions near the equator and excessive erosion from very
intense storm systems the develop in
such a hot house climate.
Intense rainfall events contribute a disproportionate amount of erosion relative to the total rainfall contribution, and this effect will only be exacerbated in the future if the frequency of
such storms increases.
The toll will continue to rise as climate change leads to more frequent and
intense tropical
storms, flooding, and extreme weather events
such as heat waves and droughts.
This allows time for preparation for
such things as higher sea levels, more
intense storms — so that the level of damage from weather events might remain constant (i.e., limited to levels for which preparation is not economically justified).
Many other measures or terms exist,
such as «named
storm days», «hurricane days», «
intense hurricanes», «net tropical cyclone activity», and so on.
The GFDL hurricane model (with a grid spacing as fine as 9 km) is able to simulate the frequency, intensity, and structure of the more
intense hurricanes,
such as category 3 - 5
storms, much more realistically than the regional (18 km grid) model.
Global warming is causing more
intense rain and snowstorms in the United States, and making extreme events
such as the January 2016 snow
storm that crippled most of the Mid-Atlantic and Northeast more likely.
Hurricanes in some areas, including the North Atlantic, are likely to become more
intense as a result of global warming even though the number of
such storms worldwide may decline, according to a new study by MIT researchers.
Scientists have long taken a similarly cautious stance, but more are starting to drop the caveat and link climate change directly to
intense storms and other extreme weather events,
such as the warm 2012 winter in the eastern U.S. and the frigid one in Europe at the same time.
No analysis has been done on the frequency of
intense typhoons (having winds of at least 50 m / s) due to an overestimation of the intensity of
such storms in the 1950s and 1960s (Black, 1993).
Leaving long - term damage in their wake,
storms such as «Super
Storm» Sandy in 2012 have rendered some coastal areas more dangerous and less desirable, lowering property values and reigniting
intense debate about restoration, new building and investment in the regions.