NewsDay (Zimbabwe)

Climate change has hit southern Africa, here is how

- Jennifer Fitchett Jennifer Fitchett is an associate professor of physical geography at University of the Witwatersr­and, South Africa

people think of climate change as a phenomenon that we will only face in the distant future. Perhaps that’s partly because climate change projection­s about rising temperatur­es and extreme weather events are tied to future dates: 2030, 2050 or 2100, for instance.

But it’s important to realise that we are experienci­ng climate change, and have done so for some time now. Over the past century, global temperatur­es have increased by approximat­ely 1°C. Sea level rise is already starting to affect certain low-lying coastal communitie­s. The world is experienci­ng more frequent and intense extreme climate events.

The Intergover­nmental Panel on Climate Change (IPCC)’s 6th Assessment Report: Physical Science basis, released last month, contains a comprehens­ive — and largely grim — assessment of the state of both recorded and projected climate change globally.

The IPCC is the United Nations body for assessing science relating to climate change — a group of expert scientists from around the world who author scientific reports on the state of the earth’s climate and future climate change projection­s.

Its latest report compiles research from 1 400 papers, and will serve as an important reference document for the COP26 meeting in Glasgow, Scotland, from October 31 to November 12. It is there that science is turned into policy.

Such policy is critical for the whole world — and urgent for southern Africa, which is particular­ly vulnerable to climatic changes. The region has already been experienci­ng climate changes that are more rapid, and with impacts that are more severe than the global average. It also struggles with a low adaptive capacity: there is little capital available for investment in measures to protect against future climate hazards, and very pressing immediate human rights needs for a large proportion of the population.

There is no avoiding the reality that southern Africa is in the throes of a climate emergency. By identifyin­g trends in the frequency of weather events happening and their intensity over a decade and exploring changes in related biological systems in light of this, it’s plain to see that the region has already been rocked by climate change and related effects.

An increase in extreme temperatur­es

Extreme temperatur­e events can be defined by the maximum temperatur­e, the deviation from the norm, or the length of time of above-threshold temperatur­es. A number of indices have been developed by the World Meteorolog­ical Organisati­on to identify and quantify these extreme temperatur­e events.

Warm events, when they meet specific criteria, are termed heatwaves. These are particular­ly dangerous for people, animals and plants, and are a direct cause of deaths.

In southern Africa, there has been an increase in the severity and frequency of heatwave events over recent decades. Interestin­gly, for a few locations, there has also been an increase in the frequency of extreme cold events. While this is not a feature of climate warming, it is induced by changes in regional climate patterns, such as the number of cold fronts which move over South Africa.

Severe drought

Drought is defined as a significan­t and prolonged departure from mean rainfall totals. The most severe, and best known, drought in southern Africa in recent years was the “Day Zero” crisis in Cape Town. While increasing pressure for water in Cape Town played a role in this, a longerterm poleward displaceme­nt in the winter-rain-bearing westerlies which bring the cold fronts and rain to Cape Town during the winter months was a significan­t contributo­r to this drought.

Southern Africa more broadly is also sensitive to El Niño-induced droughts. El Niño refers to warmer than usual conditions in the Eastern Pacific that persist for a couple of months through to years, driven by a weakening of the trade winds, and a resultant reduction in the upwelling of colder water to the sea surface just off South America. This was the cause of the 2015-16 drought in South Africa’s Kruger Park, which resulted in the drying up of watering holes, and the widely publicised death of hippos and later culling of other large mammals.

High-intensity tropical cyclones

The southern African subcontine­nt is relatively well protected from tropical cyclones by the island of Madagascar. However, some tropical cyclones do form in the Mozambique Channel, and occasional­ly some tropical cyclones move across Madagascar. These storms can — and do, as was seen most recently with tropical cyclones Idai, Kenneth and Eloise — make landfall on Mozambique.

Over recent decades, tropical cyclones in the Southwest Indian Ocean have increased in intensity; the first category 5 tropical cyclone for the sub-ocean basin was recorded in 1994.

Tropical Cyclone Idai, which bordered in intensity between categories 3 and 4 on landfall, provides stark evidence of the damage wrought by high-intensity tropical cyclones in populated areas.

There is also evidence that tropical cyclones have expanded their range polewards over recent decades, affecting a larger region of southern Africa.

Changes in the timing of phenologic­al events

In addition to the weather we experience from the changing climate itself, climate change also has an impact on biological systems.

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