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Cyclone Eloise

South-West Indian Ocean cyclone in 2021

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Tropical Cyclone Eloise on January 22, 2021
NASA · Public domain

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Through Indian Ocean, Flood and Convection

Preparations for the advancing storm took place in Madagascar before Eloise's landfall and in multiple other African countries. For Madagascar, widespread warnings and alerts were issued as the storm approached northern Madagascar. For Mozambique, high alerts were put in place for central portions of the country. Humanitarian responders prepared for response after the storms passing. Beira's port also closed for about 40 hours, and limited supplies of emergency non-food items were given. Many families were sheltered in tents at accommodation centers, and received kits for food, hygiene, and COVID-19 protection. Officials in Zimbabwe warned of ravine and flash flooding, which may cause infrastructure damage. Several northern provinces of South Africa were expected to experience heavy rains, which prompted severe risk warnings for them. Disaster management teams were placed on high alert ahead of the storm.

Extreme flooding occurred throughout central Mozambique, with many areas being flooded due to continuous heavy rains weeks prior to Eloise's landfall. More than 100,000 people have been displaced and dams are at a tipping point. Infrastructure has taken a heavy hit. Approximately 100,000 people were evacuated by 23 January, although the numbers were expected to grow to 400,000. Flooding and damage have been less than feared. Weak shelters set up for the cyclone were either damaged or destroyed. Beira was completely flooded, and the impacts were comparable to those of Cyclone Idai, though they were far less severe. Farmland was damaged as well. Teams were sent out to assess the damage and repair it. There have been 27 confirmed deaths, with one in Madagascar, 11 in Mozambique, three in Zimbabwe, 10 in South Africa, and two in Eswatini. Eleven additional people are currently missing. Current damage from the storm is estimated to be $90 million (2021 USD) in Southern Africa.

Meteorological history

On 14 January, a zone of disturbed weather formed over the central South Indian Ocean to the east of another system and gradually organized while moving westward. On 16 January, the system organized into a tropical depression. With the presence of persisting deep convection, the system eventually strengthened into Moderate Tropical Storm Eloise on 17 January. Initially, Eloise struggled to strengthen further from the presence of strong easterly shear and dry air, which caused Eloise's thunderstorm activity to be displaced to the west. Despite the presence of this shear and mid-level dry air, Eloise continued to intensify, with convection wrapping into an eye feature and outflow becoming increasingly defined, marking the intensification of Eloise into a severe tropical storm on 19 January, while heading westward towards Madagascar.

This intensification trend did not last for a long time, as Eloise made a small turn to the north and then made landfall in Antalaha, Madagascar, whilst weakening back to a moderate tropical storm, due to land interaction with the mountains of Madagascar. The next day, Eloise weakened to a tropical depression due to land interaction, with deep convection over its center eroded though it maintained flaring convection over the northern semicircle.

On 20 January, Eloise emerged into the Mozambique Channel, where Eloise began to slowly reintensify, with warm waters, a moist environment, little shear, but weak upper-level divergence contributing to the storm's slow strengthening trend. However, some upper-level convergence hindered convection from developing quickly, though all other factors were relatively favorable. Soon afterward, the upper-level convergence began to decrease, allowing the system to begin rapidly strengthening. On 21 January, Eloise's outflow became robust, though its strength was limited, due to land interaction in the northern semicircle of the storm, having the strongest winds in the southeast quadrant and sustaining much weaker winds elsewhere. Despite sustained land interaction, Eloise strengthened, with improving poleward outflow and tightly wrapped banding features wrapping into a small eye.

On 22 January, Eloise significantly improved in organization as it moved southwestward across the Mozambique Channel. Later that day, Eloise strengthened into a Category 1-equivalent tropical cyclone on the Saffir–Simpson Hurricane Scale (SSHWS), as it neared the coast of Mozambique, given the favorable conditions in the region. Early on 23 January, Eloise strengthened further and peaked as a Category 2-equivalent tropical cyclone, with 10-minute sustained winds of 150 km/h (95 mph), 1-minute sustained winds of 165 km/h (105 mph), and a minimum central pressure of 967 millibars (28.6 inHg), as the storm's eyewall began moving ashore. Soon afterward, Eloise made landfall just north of Beira, Mozambique, at the same intensity. Following landfall, Eloise rapidly deteriorated, with the storm weakening back into a moderate tropical storm within 12 hours and the eye completely disappearing. As the storm moved further inland, Eloise weakened rapidly, due to interaction with the rugged terrain and dry air. Later that day, Eloise weakened into a tropical depression as it tracked further inland. On 25 January, Eloise degenerated into a remnant low, and the MFR issued their final advisory on the system, with the storm dissipating soon afterward.

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