The Kafue Flats Experience

By Dave Lowry, Tim and Trish Broderick, Musa Lambakasa, James France, Stéphane Baugitte
Photos by Tim and Trish Broderick and Dave Lowry

The first ZWAMPS campaign consisted of both aircraft and ground surveys, these being linked most closely in the Kafue Flats region over the period Feb 2 to 5. The Kafue Flats are a floodplain wetland, extending from Itezhi-Tezhi Dam in the west, some 240 km east to Kafue town and never more than 50 km wide (https://en.wikipedia.org/wiki/Kafue_Flats). The river has changed course many times across its plain leaving scattered oxbow lakes and isolated snake-like sections of meanders to stagnate outside of flood season (Fig. 1).

Fig. 1 River Kafue lakes and meanders.

Fig. 1 River Kafue lakes and meanders.

The surveys and sampling commenced on Saturday with an intensive 4-hour zigzag flight over the region, designed by Keith Bower (Fig. 2), with elevated methane noted toward the eastern end near the start of the flight, before vertical mixing reduced these signals. The flight was very much enjoyed by Tim and our Zambian Ministry of Mines group, including Musa. Separating out the wetland source from the flight measurements and isotope data will be quite difficult because there were also numerous rural cattle herds and very extensive burning plumes producing methane (Fig. 3).

Fig. 2 End of the zig-zag flight

Fig. 2 End of the zig-zag flight

Fig. 3 Biomass burning plumes close to river

Fig. 3 Biomass burning plumes close to river

On Sunday we attempted to find our way by road to the northern margin of the Kafue Flats through the Blue Lagoon national park. After a 3-hour drive from Lusaka we reached a faded sign saying Nakeenda Lodge 9 km.  The national park sign was even more rusted. Soon we realised that this part of the park had not been visited for a long time as the track became more an overgrown and very muddy path, so we decided to sample air from a dambo in the pristine savanna (Fig. 4). The site was full of butterflies of numerous species, and even a praying mantis was catapulted into the car as we brushed past the luxuriant vegetation (Fig. 5).

Fig. 4 Stéphane directing air sampling

Fig. 4 Stéphane directing air sampling

Fig. 5 Mantis on water bottle

Fig. 5 Mantis on water bottle

Undeterred we decided to approach the park from the NW corner and reached a barrier. Here the head park ranger directed us to the managed game area and wetland.  After a few kilometres we turned off along a narrow track not on maps or GPS. Then followed 20 km over 90 minutes down a narrow and churned up track. As we passed across the invisible park boundary we came to a fishing camp on a rise above the floodplain and its associated biting insects. We were greeted by excited children and an ox cart (Fig. 6). Turns out that we were still some kilometres from the river, the resident lechwe antelope or the Game Ranger patrol camp. At this point we realised we had to get back to Lusaka before dark.

The return was no quicker, especially being interspersed with air sample collection in the pristine national park grassland (Fig. 7), as we carefully traced our way back along interweaving tracks using the GPS. We approached the outskirts of Lusaka as night fell, and on a road without lighting, carefully negotiated many minibuses without lighting and pedestrians bustling across the road to lively markets. Alarm bells had been ringing back at base when we failed to arrive back for the evening briefing and our Blue Lagoon destination was all that was known. As the city approached and phone reception returned we were able to let all know we had not broken down in the bush.

Fig. 6 Ox cart and children in the camp

Fig. 6 Ox cart and children in the camp

Fig. 7 Musa and Dave fishing for air

Fig. 7 Musa and Dave fishing for air

On Monday we had planned to sample on the south side of the floodplain, overnight in the Relax Hotel in Monze and then meet up with Mike Daly at the Lochinvar hot springs on Tuesday, but after breakfast Tim noticed that the Ford had a rear puncture from our toils the previous day, which fortunately hadn’t materialised on the evening drive back. Tim headed off hoping for a quick fix, but a brake fluid leak was also discovered from a distorted and corroded seal. Many discussions and calls later a replacement vehicle was delivered at 6 in the evening.

Plans quickly changed and the proposed rendezvous with Mike was scrapped due to the long distance, and the focus for Tuesday was to get into the sugar cane plantations and wetlands near Mazabuka. All was fine until about 2 hours into the drive when, on probably the steepest hill climb on the Kafue-Livingstone main road, there was a load bang from the rear of the vehicle. This time a major blow out and a 3 cm long rip in the tyre. Tim and Musa got to work on the jack while we jammed the other wheels with some lovely roadside calc-silicate boulders. Convoys of lorries heading for Botswana and South Africa laden with copper and other goods struggled past us. It soon became apparent that the supplied jack was not high enough for our Landcruiser, but we managed to flag down a local farmer and get the change done.

That’s when we noticed a 1cm diameter, perfectly round hole through the alloy wheel below the rip in the tyre, with a very clear entry and exit direction from a high velocity impact (Figs. 8 and 9). None of us had seen anything like that before and we still don’t know the cause, so we will leave this to your imagination.

Fig. 8 Hole in the alloy wheel – inside view

Fig. 8 Hole in the alloy wheel – inside view

Fig. 9 Hole in the alloy wheel – outside view

Fig. 9 Hole in the alloy wheel – outside view

At Mazabuka we found a tyre repairperson and then followed a wild goose chase to find a welder, then through sugar cane plantations to a market for electrodes, which then didn’t work because the alloy was wrong and required a DC current. After 2 more lost hours, we had a reality check, dumped the wheel and tyre into the back and decided to risk it on the spare and take the 30 km of dirt tracks NE toward the wetlands and river. With co-ordination of aerial images and GPS we headed down a narrow track and finally came to lush vegetation, reed beds (bulrushes) and clusters of water lilies, before the track stopped abruptly in a small clearing populated by a group of fisher folk. We proceeded to collect air samples from different heights in the reed beds. In the midst of this the reeds seemed to part and a small canoe cruised into the bank laden with good-sized Kafue bream (Figs. 10 and 11).

Fig. 10 Boatmen in the reed beds

Fig. 10 Boatmen in the reed beds

Fig. 11 Cargo of Kafue bream

Fig. 11 Cargo of Kafue bream

The drive back was far less eventful. The next morning the car hire people inspected the wheel and seemed overly keen to give us our deposit back and get us on our way. We can certainly look back on a couple of eventful and somewhat surreal days that we won’t forget in a hurry and hope that the few highly prized air samples were well worth our efforts to collect them.

Papyrus: a methane emitter and natural wind vane

The papyrus swamp measurements team
Tue 22 January 2019
Part 1

Having planned out the next few days flights – to lakes/wetlands as well as fires – and with no point refining the plans based on the weather forecast because we don’t know exactly when we will be able to start flying, I’ve joined Rebecca again to do some air sampling. This time with intent, and with a full rucksack containing anything I might need (unlike yesterday).

We are currently in a taxi out to see a contact, Steve Forsyth, who works at Mission Aviation Fellowship – Uganda, and is based at an airfield by a papyrus swamp. MAF is an organisation that operates small aircraft to transport refugees from nearby countries like the Democratic Republic of Congo or Sudan. The swamp will be a source of methane and so will be a good opportunity to work out the carbon-13 fingerprint of such an ecosystem. The principal investigator of this project, Euan Nisbet, has sampled here before, so it will be good to find out whether the fraction of carbon-13 varies over time or is very consistent.

Getting out of the conference room is a good chance to stop obsessing over ever evolving weather forecasts and see some of Uganda. And I can make myself useful by taking photos of the sampling location at very least.

Part 2

We are on the way back from the airfield now. It was completely surrounded by papyrus swamp, which meant we could access it quite easily. We were escorted around the airfield by Ivan, who was essential in helping us not get our feet wet (we were not keen to lose a trainer in the swamp!) while getting as close to the swamp as possible.

The papyrus plants were extremely tall in places – close to 4m probably. Some areas were cut down to the stem, and they grow back in about a month according to Ivan. The stems themselves are very strong, and are excellent wind vanes of you ever are in need of one. Which I did, as I was taking wind measurements to accompany the air samples.

In all, we took 13 samples from locations close to the surface of the water up to about 2m high, all around the edge of the swamp, plus one background sample further away from it. This will allow us to find out the carbon-13 fingerprint of this papyrus swamp, where there were the highest methane concentrations. For example, the papyrus that was cut down to ground level may emit more or less methane than the fully grown area and maybe the measurements will give us an indication of that.

 

There is no science without coffee

Ethiopian Coffee

Without coffee, there is no science

I write this at 8am on a Sunday in a bustling airport in Addis Ababa, with a few hours to spare before my connecting flight. I had intended to prepare a background post outlining the plan for the field work and the wider project, but doing  anything non-essential in the run-up to the trip proved a little over-ambitious.

A colleague and I are flying out to Entebbe, which is on Lake Victoria in Uganda, about 30km away from Kampala, to join the rest of the detachment team to work on the FAAM research aircraft. We took a red-eye flight from London and as a result I really needed the excellent Ethiopian coffee I just finished. We were supposed to start the research flights tomorrow, but the final sign off has not yet been obtained from the local officials – not for want of trying! So instead, today is a “hard down day”, meaning no access to the research aircraft at all, because without the sign off, we can’t get airborne.

So Monday will be used to get all the instruments up and ready while the aircraft remains on the ground and hopefully Tuesday we will get airborne. We really have a packed schedule, as we are only doing MOYA flights Tuesday to Friday and then one more on Tuesday next week (another project called HyVic is flying over Lake Victoria on the intervening days). The shorter detachment saves on costs, but means we are at the mercy of the weather. To make sure we can fly every day we have several different flight options to choose from: Lake Victoria, Lake Kyoga, Lake Wamala and wildfires in northern Uganda. We will pick one of these based on which location has the best weather conditions, and fingers crossed we have time to do 2 of each. We also hope to circuit Kampala to sample the city’s emissions as part of one of the flights.

Why are we going to all this effort? Mainly to figure out how much methane is coming out from the lakes, wetlands and wildfires. This will help us to piece together the global methane trends – a key factor in how much the planet will warm in the coming years. To do this, we sample the methane in the atmosphere while airborne, as well as ethane and other pollutants. Some of these measurements come in real time, others are taken back to the UK to analyse for carbon isotopes, which gives us a clue as to the emissions source. You will find blogs from our 2017 airborne field work, based in Senegal, where wildfires were sampled. I have to say, based on the turbulence we felt on the commercial flight here, I am not too keen on flying near wildfires (which cause turbulence from their heat) or storms (which are quite common even though this is the dry season for Uganda).

I think the boost from the coffee is wearing off now, so I will sign off from my first post. There will be more content over the coming week, when I hope to have more than a few hours doze before sitting down to write.

Ponds in the Pantanal

Our next post from the field comes from Luciana Gatti and Manuel Gloor, who have been measuring how much methane is found over the Pantanal region of Brazil. This is a huge area of wetlands, and is therefore also a huge source of methane. 

 

Luciana Gatti and Manuel Gloor with the pilots of the light aircraft

Luciana Gatti and Manuel Gloor with the pilots of the light aircraft

We, Luciana Gatti and Manuel Gloor, have just returned from the Pantanal area where we have started sampling of the vertical air column (0 to 4.5 km height above sea level) using light aircraft (see the first photo) for subsequent analysis for CH4 at Luciana’s laboratory.
The mosaic of circular ponds in the Pantanal

The mosaic of circular ponds in the Pantanal

The Pantanal is one of the largest wetlands worldwide with an areal extent on the order of 150,000 km². It is a flat area which drains very slowly via a complicated system of ponds feeding each other as well as some slowly moving rivers. The region is seasonally flooded and has seen major precipitation maxima in recent years but also sometimes drier phases. It is a potential candidate region for a climate change methane emissions feedback.
An area of flowing water in the Pantanal

An area of flowing water in the Pantanal

The mosaic of circular ponds can be very clearly seen from the aircraft (photo 2) as well as occasionally flowing water areas (photo 3). If one looks really, really carefully one may even spot a hungry caiman or two. The vertical air profile has already been analyzed for greenhouse gases and reveals a major methane source which reveals itself as a large concentration enhancement within the lowermost 2 km above ground.