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15 February 2021 | Story Supplied | Photo Supplied
Dr João Vidal is a research fellow at the Department of Plant Sciences and the Afromontane Research Unit (ARU) at the University of the Free State (UFS).

According to United Nations data projections for 2100, sub-Saharan Africa is set to experience a demographic explosion. The most rapid population growth zones in Africa are in or around mountains and the importance of managing these mountain ecosystems sustainably in order to maintain the benefits to such a growing population is critical, says Dr João Vidal, a research fellow at the Department of Plant Sciences and the Afromontane Research Unit (ARU) at the University of the Free State (UFS). 

The link between human population growth and the demand for water will impact these mountain grasslands. All of Africa’s important rivers originate in mountainous areas. The sustainable management of African mountain landscapes is thus vital for the sustained provision of quality water in suitable quantities. “Water is already limited in some places. This year we are facing another drought in South Africa, and if it was not for the mountains, it could have been much worse. The long-term resilience of Southern Africa’s mountains and their ecosystem services should be an absolute priority for both research and conservation,” says Dr Vidal.

Human population growth has several implications

As a mountain ecologist, his recent research is centred on developing indicators for monitoring biodiversity change in Southern Africa’s mountains. This is a collaborative research project with the South African Environmental Observation Network (SAEON), Ezemvelo KZN Wildlife, and the University of Pretoria.

Human population growth, as predicted for Southern Africa, has several implications for natural-resource management and biodiversity conservation. “Southern Africa has one of the highest proportions of grassland-dominated mountains in the world, comparable only to Central Asia,” says Dr Vidal. 

In December, UN Secretary-General António Guterres said during the launch of the 2021 Global Humanitarian Overview: “Conflict, climate change and COVID-19 have created the greatest humanitarian challenge since the Second World War. The number of people at risk of starvation has doubled. Hundreds of millions of children are out of school. Levels of extreme poverty have risen for the first time in 22 years.”

According to Dr Vidal this new scenario significantly increases the pressure on mountain environments and their biota, since people will have to find alternative ways of feeding their families, their animals, while the economy struggles to recover globally.

Through his research, Dr Vidal – together with a growing community of practices for Southern Africa’s mountains – aims to understand the socio-ecological functioning of these montane grasslands in order to encourage a science-policy-action interface for their sustainable management in a changing world. 


Alternative ways for measuring environmental change in mountains

Since much global mountain research is focused on forest-dominated mountains, Dr Vidal and his collaborators are developing specific tools to track climate change in grassy mountains.
He explains: “When you look at the available tools for tracking climate change in mountains, you have a tree line for many mountains in the world. However, with the Southern African grassy mountains, it is impossible to use such a tool. We are working on alternative ways for measuring environmental change in our mountains.

“As it gets warmer, certain communities of grasses may retract towards higher elevations because they need a certain minimum temperature to survive. The problem seems to be that current climate change is occurring at a much faster rate than most species might be able to retract. This means that higher temperatures may lead to habitat losses for temperature-vulnerable groups.

“Climate change is also making mountains increasingly vulnerable to ecological invasion by non-native species. The severe temperatures in mountains are a good barrier for many problematic lowland species. But with warmer temperatures in the mountains, these barriers are being weakened, increasing the number of potentially invasive plants in our mountains. With higher temperatures there is potential for a large guild of invasive trees to overrun grassland mountains affecting waterflow into dams and rivers. Examples are pines, willows, gums, and wattles, to name a few.

“The presence of invasive trees, especially along rivers, has long-term negative impacts on the functioning of mountain catchments. These trees destabilise riverbanks, extract large amounts of water, and cause local extinction of endemic montane biodiversity. In drier environments such as grasslands, this exacerbates the fragile water productivity,” he adds.

Global policymakers to recognise the value of grassy mountains 

It is important to draw attention to the value of natural grassy mountain systems around the world and to how threatened they are. The world’s grassy mountains need to be better studied and better placed on the global stage. This will encourage policy makers to recognise these systems and implement appropriate measures to facilitate their sustainable management. 

For the first time in 20 years, the recent International Panel of Climate Change (IPCC) report to the United Nations included a chapter focusing solely on mountains. “Policymakers are finally realising how disproportionately important mountain environments are and how dramatically they are affected by climate change,” says Dr Vidal. 

However, African mountains are underrepresented in research literature; it is the only continent for which there is no data included in the IPCC report. There is an urgent need to represent African mountains – especially Southern Africa’s mountains – on the global stage when it comes to climate change,” states Dr Vidal.

Dr Vidal is conducting this study in partnership with Dr Ralph Clark, Director of the ARU on the UFS Qwaqwa Campus

News Archive

The influence of load shedding on the evening timetable
2008-01-31

The load shedding that is being applied at present also has a certain influence on especially the evening module and venue timetable. As part of the contingency planning of the UFS, an alternative module and venue timetable has been compiled so that classes that cannot take place during evenings in the week as a result of load shedding can be accommodated on Fridays and Saturdays.

After consultation with students, lecturers will decide whether the alternative timetable will apply when load shedding does indeed occur or whether the alternative timetable will be a permanent arrangement.

The alternative evening module and venue timetable are as follows:

Classes that are presented in the timeslot 18:10 to 21:00 on Thursdays are alternatively accommodated in the same venues at the same times on a Friday. Double or more periods that commence at 17:00, but continue into the period of load shedding are also included in this alternative arrangement.

It is important to note that lecturers who present double periods that start at 14:10 and continue into the period of load shedding must make ad hoc arrangements should they wish to have their periods also included in the alternative timetable.

Classes that take place in the timeslot 20:10 to 22:00 on Wednesdays are alternatively accommodated in the timeslot 08:10 to 12:00 on Saturdays, in a few cases in different venues from those scheduled initially. Double or more periods that start at 18:10, but continue into the period of load shedding are also included in this alternative arrangement.

The venue changes for Wednesday periods that are accommodated on Saturdays are as follows:

  • BLG114 Practical 1 English (A) in the Biology Building 28 from 08:10 to 11:00
     
  • STK114 Practical 1 Afrikaans (D) in West Block 201 from 09:10 to 11:00
     
  • STK114 Practical 1 English (D) in West Block 202 from 09:10 to 11:00
     
  • ALM108 Lecture 1 English (G) in FGG169 from 09:10 to 11:00
     
  • EKN314 Lecture 2 English (A) in the Rindl Hall from 09:10 to 11:00
     
  • EFA112 Lecture 2 Afrikaans (A) in FGG377 from 10:10 to 11:00
     
  • EFK112 Lecture 2 Afrikaans (A) in FGG183 from 10:10 to 11:00
     
  • DLS112 Lecture 2 English (A) in FGG184 from 10:10 to 11:00
     
  • ALC108 Lecture 2 English (E) in the South Block 1 from 10:10 to 11:00
     
  • DLS112 Lecture 2 Afrikaans (A) in the FGG377 from 11:10 to 12:00
     
  • EFA112 Lecture 2 English (A) in FGG183 from 11:10 to 12:00
     
  • EFK112 Lecture 2 English (A) in FGG184 from 11:10 to 12:00
     
  • ELF112 Lecture 2 English (A) in FGG169 from 11:10 to 12:00
     
  • EKN214 Lecture 3 English (A) in Stabilis 4 from 11:10 to 12:00

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