Growing cyclones in the Arabian sea

Recently, the growing frequency of tropical cyclones in the Arabian sea has surprised climatologists and scholars.We know that cyclogenesis in the North Indian Ocean, particularly in the Arabian sea hardly take place. However, the origin of cyclones “Kyarr” and “Maha” within a week is signalling something abnormal that deserves greater attention. The proper understanding and analysis of causes behind cyclogenesis is highly essential to cope with the possible damage of unseasoned disasters. Likewise, in this blog, “Growing cyclones in the Arabian sea” I am going to explain some of reasons responsible for the ongoing natural calamities.

What is tropical cyclone ?

Tropical cyclone is the most disastrous climatic phenomenon generally occurs around the low pressure in the tropical regions of the oceanic water. For this, temperature, humidity, and low pressure area are the most important conditions as it uses the moist air as a fuel for the typical climatic engine.

As usually, such systems are being formed in the proximity of equator and coastal regions. In the world, these are known by different names as per the regional identities like, hurricane, tornado, and typhoon etc.

According to the intensity and severity of cyclones, cyclone rating agencies based on the parameters of world meteorological department, classify all originating cyclones in the five categories. Recent Kyarr and Maha are classified as 4th and 3rd categories. For the North Indian Ocean, Indian meteorological department uses seven categories to rate the cyclone in question.

Causes of cyclogenesis in the North Indian Ocean

As I mentioned earlier that humid and moist air is the driving force behind the cyclonic phenomenon. And, Inter-tropical converging belt that originates in the north of equator in the summer season, is highly instrumental in the onseting of monsoon over the Indian subcontinent.

ITCZ is a low pressure belt which migrates seasonally in the north and south of the equator. Logically, it crosses twice in a year–with the advancement of summer and with the beginning of retreat. Therefore, the ideal conditions for the formation of cyclones in the North Indian Ocean get developed in the month of may/June and October/Nov.

In the Indian subcontinent, data suggests that the frequency of cyclones has been observed with the advancement and retreating phases of the monsoon.

Why is  cyclogenesis absent during the monsoon period ?

Though the effects of tropical cyclone are beyond the managing capacity of human beings and sound so destructive, it requires wind free atmosphere at the higher level (or low wind shear) to develop and strengthen it properly.

Otherwise, in case of stronger wind at the higher level in the form or jet stream or monsoonal wind, it cannot sustain longer and gets easily disrupted. If the wind shear is strong, the dry air replaces moist, humid air which is highly essential for the cyclonic phenomenon.

During monsoon, the strong wind prevents the formation of required conditions in the North Indian Ocean. Hence, the cyclogenesis in the North Indian Ocean during monsoon remains absent. This is the reason why the frequency of cyclones is mainly observed in the pre-monsoonal months, as well as during retreating phases.

In the absence of strong wind generated by monsoonal phenomenon, tranquility returns favouring cyclogenesis in the May and October months.

Why the difference in cyclogenesis in the Bay Of Bengal and Arabian Sea ?

In the Arabian sea compare to Bay Of Bengal, the wind shear phenomenon is stronger so it inhibit the formation of ideal conditions for cyclogenesis. Apart from this, the dry air that blows from the western Thar desert prevents the formation of cyclones as the moist, humid air act as fuel to develop, sustain and strengthen the tropical cyclones.

Moreover, the global climatic changes have also profound impacts on the formation. Whereas, in the Bay Of Bengal the conditions are opposite of the Arabian sea. These are some reasons that  make the difference between Arabian Sea and Bay Of Bengals in terms of cyclogenesis.

 Then, why the frequency of cyclones in the Arabian Sea..

The concrete and concluding evidences are yet to be recognized about the recent growing cyclones in the Arabian sea, but  the common consensus is gaining momentum in favour of impacts of man made climate change.

In the summer season, in the region of marathwada, as well as other parts of the Maharashtra, Karnataka, and other western Indian states were reeling under unbearable drought and water scarcity problem and now these are the same region which are being washed away by the heavy rains and catastrophical unseasoned cyclones.

The abnormal extremity of droughts and devastating floods are the clear-cut manifestation of impacts of climate change and for that we need to prepare. Undoubtedly, in the agriculturally predominant regions of the developing countries, such impacts of climate change have greater affecting capacity.

Recently, in the  Maharashtra and other western states of India where kharif crops were on the verge of ripping, the Kyarr and Maha cyclones damaged the entire standing crops, is self evident.

Here whom to blame ?–nature, human ignorance, or procrastination… But, in the coming days,  one thing is going to be inevitable and that is unpredictability of climate, as well as nature..

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