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2019–2022 locust infestation

Locust outbreak in Africa and Asia

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Through Arabian Peninsula, Indian subcontinent and Kenya

The locust infestations began when Cyclone Mekunu in 2018 produced heavy rains in the Rub' al Khali of the Arabian Peninsula; in spring 2019, swarms spread from these areas, and by June 2019, the locusts spread north to Iran, Pakistan, and India and south to East Africa, particularly the Horn of Africa. By the end of 2019, there were swarms in Ethiopia, Eritrea, Somalia, Kenya, Saudi Arabia, Yemen, Egypt, Oman, Iran, India, and Pakistan. By June 2020, a separate swarm appeared in South America, affecting Paraguay and Argentina.

In April 2020, travel and shipping restrictions precipitated by the spread of COVID-19 began to hamper efforts to control the locusts, preventing the transport of pesticides, equipment, and personnel, and contributing to the global incidence of COVID-19 related food insecurity.

Locust swarms worldwide faced a steady decline in size from May to October 2020, as countries and intergovernmental organisations instituted extensive aerial and ground pest control efforts, aided by low quantities of rainfall in several affected regions, as well as the absence of storm activity in the Indian Ocean. By October 2020, Ethiopia, Eritrea, Somalia and Yemen continued to harbour significant swarms of locusts, with the remainder situated in isolated pockets of Kenya, Sudan and Saudi Arabia. Locust swarms continued to threaten countries around the southern Red Sea and Gulf of Aden, as well as their immediate neighbours, until February 2022 when the surge was officially declared to be over.

Causes

When periods of heavy rainfall follow periods of relative drought, solitary desert locusts emerge to feed on new-growth foliage and lay eggs in the newly moist soil, which prevents them from drying out. The sight and smell of other locusts, as well as sensory stimulation from contact between locusts' hind legs, precipitates changes in the locusts' behaviour and morphology; the previously green, nocturnal and solitary creatures become larger, develop black-and-yellow colouring, and begin to seek out other locusts, a process known as gregarization. These changes result in the formation of large locust swarms that gregarize nearby locusts and breed profusely, allowing them to undergo rapid, exponential growth. The swarms proceed to feed on the newly abundant vegetation, making use of improved swarm coordination, the result of larger brain sizes, as well as increased range, the result of increased metabolic activity, larger muscles, and longer wings, to travel up to 130 km a day in search of new vegetation and moist weather, often propelling themselves by the wind.

This particular desert locust plague traces back to May 2018, when Cyclone Mekunu passed over a vast, unpopulated desert on the southern Arabian Peninsula known as the Rub' al Khali, filling the space between sand dunes with ephemeral lakes, which allowed locusts to breed undetected. This was exacerbated in October 2018 by Cyclone Luban, which spawned in the central Arabian Sea, moved westward, and rained out over the same region near the border of Yemen and Oman. The Indian Ocean Dipole, an irregular oscillation in sea surface temperatures between the western and eastern parts of the Indian Ocean, has increased in magnitude due to the effects of climate change. This shift has resulted in increased cyclone activity over the last decade in the Persian Gulf, previously home to very few cyclones, and is associated with flooding in countries along the western Indian Ocean, dry weather in the east, and bushfires in Australia.

The two cyclones created conditions conducive to mass locust reproduction, enabling three generations of locusts to breed over a nine-month period, which increased their number in the Arabian Desert roughly 8,000-fold.

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