Published: October 30,2015
Chapala rapidly intensified and had estimated winds as strong as a high-end Category 4 early Friday. Some further decrease in intensity are expected over the next day or so as the system gradually weakens.
Cyclone Chapala: Current Status
(MORE: Why Tropical Cyclones Are Named)
Warmer-than-average Arabian Sea water along its path had, in part, allowed for Chapala is intensify so rapidly.
Impressive outflow channel N of Cyclone #Chapala. Shows the fine line between being sheared apart & possible RI.
Cyclone Chapala's Forecast Path
In this case, we expect Chapala to make landfall as a weaker, possibly much weaker cyclone than its potential maximum intensity over the Arabian Sea. Small tropical cyclones can both intensify rapidly and weaken rapidly.
However, Chapala may still be a formidable cyclone of at least Category 1 intensity at landfall, a very unusual, if not unprecedented occurrence for Yemen or southwest Oman. (More on that below.)
The threat of heavy rainfall should be in play regardless of the intensity.
Chapala has the potential to dump 3-4 times or more the average yearly rain in just a day or two over parts of eastern Yemen and southwest Oman. According to worldclimate.com, the average annual rainfall in Salalah, Oman (estimated population 197,000 as of 2009), is only around 4 inches.
Model Rainfall Forecast: Cyclone Chapala
(INTERACTIVE: Oman/Yemen Coast in the Path of Chapala)
Rivers running from these mountains that are normally dry or feature very low flow would see rapid rises with rainfall of this magnitude, which could be destructive or deadly.
Unprecedented Landfall?
You may wonder how often "tropical cyclone" and the "Arabian Peninsula" appear in the same sentence. How unusual could Chapala be?First, according to hurricane specialist Michael Lowry and the NOAA best track database, there is no record of a hurricane-strength cyclone landfall in Yemen dating to 1945.
#Chapala forecast to hit Arabian Peninsula as only 3rd hurricane strength landfall on record. Big rains to dry area.
(WUNDERBLOG: Cyclone Chapala's Yemen Threat)
Secondly, there has been only one Category 5 equivalent Arabian Sea cyclone of record, Gonu in 2007, which weakened before making landfall in northern Oman near the capital, Muscat. Weather Underground's Dr. Jeff Masters notes, however, that reliable satellite estimates in the Arabian Sea date only to 1990.
There is no record of a cyclone of Category 4 strength or stronger tracking as far south as Chapala in the Arabian Sea.
(MORE: Hurricanes in Strange Places
Despite all this, Arabian Sea tropical cyclones are not as unusual as they sound.
Each year, an average of one to two tropical cyclones form in the Arabian Sea, according to a 2011 climatology study by Amato Evan and Suzana Camargo.
Tracks
of all recorded global tropical cyclones from 1851-2008. Tracks in the
Arabian Sea are highlighted by the yellow box. (NOAA/NCDC)
These cyclones are most likely to form in two periods: from May through June and October through November. The mid-late summer period is typically not favorable, thanks to increased wind shear from the wet phase of the Asian monsoon.
(MORE: Where the Season Peaks Twice)
In June 2007, Cyclone Gonu was the most intense Arabian Sea storm on record, making landfall in Oman, then in southern Iran.
Gonu claimed 100 lives in Oman, Iran and the United Arab Emirates and was responsible for $4 billion in damage, according to the Evan and Camargo study.
Almost exactly three years later, Cyclone Phet alarmingly intensified to a Category 4 equivalent cyclone, before weakening to a Category 1 storm upon making landfall on the eastern tip of Oman, east of the capital city of Muscat.
In May 1999, Cyclone ARB 01 slammed into Pakistan near Karachi as a strong Category 3 equivalent storm, killing at least 700 in Pakistan. This was the strongest tropical cyclone on record to hit Pakistan.
(MORE: Deadliest Tropical Cyclones in World History)
In the limited historical record, however, strong cyclones in the Arabian Sea are more rare than other basins, due to the proximity of dry air from the Arabian Desert, the aforementioned increased wind shear during the wet phase of the Asian monsoon, and the basin's overall small size.
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