An onset in Kerala is said to be bogus when atmospheric conditions resemble the monsoon but are improper and short-lived. The IMD has a
criteria for declaring the monsoon’s onset in Kerala which gives equal importance to rainfall and winds. In addition to this, an important identification of the monsoon’s arrival in Kerala is the presence of well-defined and strong cross equatorial winds. These cross equatorial winds are an integral part of the monsoon circulation. They transport moisture from the Southern Indian Ocean to India. They blow across the equator and earth’s rotational effect changes their direction after crossing the equator, hence the name "cross equatorial winds". The left part of above figure shows proper, "C shaped" cross equatorial winds (circled red) around June 5, 2015 when the monsoon had arrived in Kerala. The right part of the image shows present situation in which there is an absence of "C shaped winds", thus indicating an absence of proper cross equatorial winds.
Such bogus monsoon onsets generally occur in the month of May, during the years when the monsoon is going to be delayed in Kerala. Any strong low pressure in the Bay of Bengal (such as a tropical cyclone) attracts the winds (such as from Southern Indian Ocean and Arabian Sea) towards itself. This leads to an increase in the winds in the Arabian Sea and Bay of Bengal thereby leading to illusionary monsoon-like conditions. However, after this low pressure disappears, these conditions also disappear. Last week, the Bay of Bengal witnessed a Tropical Cyclone named Roanu. It moved along the east coast of India and made landfall in Bangladesh on May 21. Its presence has lead to an increase in westerly winds all over the Arabian Sea and Bay of Bengal, thus creating monsoon-like perturbations. These perturbations are the main reasons of a disagreement among forecasters regarding the monsoon’s onset dates.
Monsoon’s onset likely to be delayed in Kerala
A cyclonic circulation (low pressure) will form at an altitude of around 20,000 feet over the Central Arabian Sea. As a result of this low pressure, precipitation will commence in the central Arabian Sea along with the western coast of India. In addition to this, the thundershowers expected in parts of Kerala, Tamil Nadu, Karnataka, Andhra Pradesh this week are pre-monsoon showers.
As per the models, the cross equatorial winds aren’t going to strengthen and organise (to the required extent) in the remaining days of May and hence it is unlikely that there will be an early or even timely onset of the monsoon in Kerala. According to the long range models, these winds will properly organise after June 3 and depending on the rainfall activity at that time (which is difficult to forecast now), the monsoon will reach Kerala most likely in the second week of June. The exact date will become clear once June commences.
This can cause some delay in the further progress of the monsoon, especially in Central India. It will be too early to comment on the onset picture in North India. But high temperatures and some heat waves are expected to continue in the plains of North India, Central India and parts of East India in the remaining days of May.