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blowing in the wind: how hurricane ophelia became a very big deal - air cooler working without water

by:HICOOL     2019-07-20
blowing in the wind: how hurricane ophelia became a very big deal  -  air cooler working without water
It was a surprise for many people.
After all, we consider hurricanes to be part of the tropical world, including the Caribbean and southern United States, but far from Ireland and western Europe.
Normally, Atlantic hurricanes form between five to twenty degrees north and south of the equator, and when the sea surface temperature exceeds the depth of 27 degrees Celsius to dozens of meters, it is far enough from the equator, can kick in.
Initially, Atlantic hurricanes tend to travel west to the Caribbean and the Americas, which consume the most energy.
Some travel north in the Atlantic Ocean, some travel north on the east coast of the United States, but only a few will cross the Atlantic Ocean back to Western Europe, and fewer people will reach the coast.
It formed about 300 km kilometers southeast of the Azores, initially staying in the area for a few days, intensifying into a category three hurricane, the strongest hurricane recorded in the Far East satellite era.
It then tracks northeast directions that affect Portugal, Spain, and France, then crosses western Ireland third, the northern continent of Scotland, Norway, Sweden and Finland, and finally crosses Russia.
Due to its entry into colder waters and the effects of land friction on it, it is constantly losing its strength.
Ofiya is unusual in many ways.
This is the only season to do so since 1893.
During this period, only a small number of hurricanes were not tracked west of the Atlantic Ocean.
There are also some unusual features in Ireland.
It's a big system, and it's still more than 1,000 km in diameter when it hits Ireland.
The minimum central pressure of the storm eye is 962. 2 hundred PA in Co
Kerry and this helped create a very strong wind.
The highest gust recorded was 156 km/h.
10 metres of Cork in standard height.
However, the agust 191 kmph Fasnet Rock Creek is recorded on a non-
The standard measuring height of 61 m is the highest wind speed in Ireland's history.
At Roches Point, the average wind speed of up to 10 minutes was 111 kilometers, setting a new record in October, the eighth-highest sustained wind speed in history.
These strong winds and low central air pressure helped to produce very high waves and created a new temporary record of Level 26. 1m (85. 6 feet)
It was recorded near the Cork coast.
The temperature associated with this storm is very high, this is a typical hurricane, its center is relatively warm, unlike the Middle
There are relatively cold latitude storms in the center.
The highest temperature is 19.
4 degrees Celsius was recorded at the Co. Valentia Observatory
Kerry, this is about five degrees above the long-term average.
Ireland is often affected by the surplus tropical remnants of the Atlantic hurricane.
This happens not every year, but with record rainfall and record-breaking winds.
Most of these remains have not been noticed, as they are only periods of strong winds and rainfall that are not within the range of Ireland's annual weather that usually occurs.
Ireland and Europe are likely to be increasingly affected by the remnants of the hurricane.
Hurricane Atlantic moved further north, while the prerequisites for maintaining strength gradually increased as sea levels rose
Surface temperature, which is the main reason for their formation.
In addition, hurricanes tend to move towards the warmest waters, which helps push north as the ocean and air that is caused by global warming heats up.
An interesting and possible diagnostic aspect of these weather events is their early days as they occur outside the normal storage section of late autumn/winter/early spring this year.
The peak of the Atlantic hurricane season is usually in the middle.
On September, Hurricane Debbie took place on September 16, Hurricane Charlie took place on August 25, and Hurricane ofiya took place on October 16.
This means that other historical storms that have affected Ireland in these months may actually be an additional tropical remnant of the hurricane.
The storm of August 23, 1680 destroyed many ships around the Irish and British coasts, and according to an analysis of the vessel log for that time period, the storm was linked to the remnants of the hurricane.
An example of a possible storm is the storm of July 30, 1698, which is recorded in Limerick and is so powerful that it stops Shannon's tide.
Orphia caused death and destruction in Ireland and elsewhere.
Three people in Ireland were killed directly by falling trees.
The other two died while repairing the damage caused by strong winds.
Strong winds recorded in Portugal and Spain have intensified and extended the wildfire that killed 49 people.
The loss in Ireland was considerable, with a large number of trees being cut down and resulting in power outages that affected 360,000 people during peak periods.
Many people have no water for a few days.
Buildings, including private homes, schools and stadiums, were severely damaged.
While the total cost of insurance for this event may exceed EUR 100 million, the real cost is much higher because not every damage is covered by insurance.
Devastating tail
Hurricanes like Debbie, Charlie, and ofiya will still be rare, and Ireland has yet to experience hurricanes that bring both extremely high winds and rain.
Just five days after the ofiya incident, the storm that affected Ireland Brian also had tropical origins east of the Caribbean, and then usually moved northeast towards Ireland, causing further damage in Devon, England, even one person died.
Because Ireland is in a dynamic weather environment, we should never be surprised by the consequences that this may have for us.
Even without the effects of climate change, we can expect cold weather from the north or east, or storms or Hurricane sites from the west or southwest.
Nor should we underestimate the potential impact of these events.
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