Now that it’s Autumn Ireland is suffering some very damp weather, and Wicklow is experiencing a ‘classic’ Autumn, cold wet and muddy, but quite beautiful too. This is largely the result of two very warm and balmy summers in a row – not in Ireland but in Africa, in the Sahara Desert. After hot summers in North Africa huge amounts of dust are blown westwards out into the Atlantic Ocean.
Some of the dust is carried northwards directly into the Bay of Biscay to the south of Ireland, but most goes to Brazil in South America and the Caribbean. Some of the dust lands on the Brazilian coast where it has been directly identified as damaging the rare coastal cloud forests. Much of it lands in the Caribbean where it sinks to the sea floor and smothers coral reefs, in some cases directly killing them.
The lighter dust that doesn’t land on the sea begins to do something quite different. At the heart of every single drop of rain lies a tiny particle of dust. Water molecules evaporating from the ocean are attracted to this dust and slowly begin to collect around it. The dust is carried from the Caribbean on the air currents that flow above the Gulf Stream, the same current that keeps our temperatures mild despite the fact that the island of Ireland lies very far north. When they arrive over Ireland’s southern coast the combination of cold land air and the fact the droplets are too heavy to stay airborne causes them to fall in torrents, sometimes causing terrible flood damage to coastal communities in the south west.
The rains of autumn are going to get worse over the years, for the simple reason that the Sahara is expanding at ‘an alarming rate’. How and why this desert originally began to form throusands of years ago is still something of a mystery, but the cause of its rapid expansion in the 20th and 21st centuries is not a mystery – UN studies have found that it is largely due to cattle-farming in sub-Saharan Africa.
Areas around water sources begin to suffer extreme climate change and erosion because grazing animals congregate within only a few hours walking-distance of them. These 10-12 km desertification circles around drinking wells were identified and termed “Piospheres” by an Australian ecologist, Dr. Robert Lange, as early as 1969. The width of these desertification circles exactly matches the distance that a bovine animal can travel in one night . The big problem now is that the population of sub-Saharan Africa has grown and led to a demand for more and more cattle, which has caused the Sahara to grow faster and faster.
So the secret to solving this problem can only be a change in farming practices, which will require a cultural change and the developments of new methods of irrigation to restore the damaged environments of sub-Saharan Africa.