Returning to education after many years, CAT student Tammi Dallaston discovers a whole new world of learning.
In the UK, gardens cover more land than nature reserves, so what we do in them matters. Alex Chadwick shares some tips on creating your own little wildlife haven.
As week two at COP23 begins, new leadership becomes ever more vital – Paul Allen reports from Bonn.
My second week at the COP23 UN climate talks has now begun. This is normally the time when the deeper negotiations begin. This has become increasingly urgent – this morning the Global Carbon Project revealed that, after three years of levelling off, humanity’s global carbon emissions are on the rise again.
At the UN climate talks in Bonn Paul Allen finds the USA to be a surprising source of inspiration.
Published just before COP23, the UN Environment Emissions Gap Report was the subject of a major presentation in the German Pavilion. It shows that the gap between commitments made in Paris 2015 and what’s needed to keep within ‘safe’ levels of global temperature rise ranges from 11 gigatons (for an increase of 20C) and 19 gigatons (for 1.50C) of CO2 equivalent. That’s a huge gap.
With CAT’s annual conference fast approaching, programme organiser Tanya Hawkes gives us a taste of what’s in store.
How three people are shaping a more sustainable world, in their own words…
Imagine a world where we have broken our ties with fossil fuels… Our towns and cities are awash with innovative practical projects that are rebuilding our relationship with food, energy, transport and buildings, openly supported by the wider economic and political systems. Such innovation has unleashed all kinds of co-benefits, from cleaner air to better diets, more jobs and income arising across the local area.
This half term, come and join the fun at CAT
Ride the water powered funicular railway up to the site, before beginning your adventure.
With free children’s activities, you could be learning about sustainable living while the kids build a solar boat, make natural jewellery, or plant their own beanstalks. There are free guided walks every day throughout the half term week, too.
The Visitor Centre is looking great at the moment, with new signage being developed and new displays being worked on. The gardens are a joy to behold, and you’ll get a chance to have a peek at Carwyn Lloyd Jones’ tiny caravan, as featured on George Clarke’s Amazing Spaces.
Finally, after all that exploring, visit the CAT restaurant for a filling lunch or a delicious cake. It’s all veggie, with lots of vegan options, and we cater for specialist diets too.
Book here to get 10% off your ticket price.
Looking forward to meeting you!
“Well, maybe you do just eat a little bit too much…” said Laura’s (very tactfully!) when I queried her, slightly exasperatedly about my diet once I’d fiddled around with it in Laura’s Larder – the new online tool about healthy and sustainable diets launched today at CAT. The idea is, you fill in what you might eat during a week and then it tells you the nutritional values of your diet – kilocalorie (energy), protein, fats, salts and micronutrients; and the greenhouse gas (GHG) emissions resulting from what you eat – ‘farm to fork’. Then, you can make changes to try to make your diet healthier, and lower in emissions.
We got a sneak preview as staff here at CAT and I’d had a bit of time to play around with it, but was having trouble ticking the ‘daily kilocalories’ box. It kept on telling me, basically, that I was eating too much.
I started out being quite honest about what I eat. I hadn’t kept a diary of my diet, but I thought about what I’d usually eat for breakfast every day, and filled in some examples of the things I might eat for lunch and dinner, together with the additional snack I have when I get home from work and the multiple cups of coffee that I sprinkle through mid-mornings. I’d included a few drinks of an evening (that I was right in suspecting was too many!), a bit of chocolate here and a portion of chips there. I generally eat pretty large portions of food, and I probably have a fry-up once on a weekend, and a (pretty disgustingly giant, but home-cooked, so obviously more healthy!) sunday roast.
Having worked on the Zero Carbon Britain project here at CAT for a couple of years, the first thing I noticed was that the GHG emissions from my diet were pretty high. I have picked up a couple of things whilst working with Laura herself on the food and diets model in Zero Carbon Britain: Rethinking the Future, and on the new report linking diets, GHG emissions and land use: People, Plate and Planet.
I knew that the culprit was probably cheddar cheese. I don’t eat meat (red meat is especially high in emissions), but I do like cheese. Since beef and milk come from the same animals (something I, surprisingly, had not thought about ever before in my life!), I knew that the GHG emissions from hard cheeses like this were almost as bad as those from the meat. So, I started cutting out some cheese from my ‘diet’ in the application (I have been trying to do this in real life too). But I was surprised about the next two things that contributed to my high GHG score – cider (yes, I drink too much of it), and broccoli. Broccoli?! “But its a nice green vegetable, and my mum always used to encourage me to eat it when I was little – its good for you!”, I exclaimed at my computer screen. I challenged Laura: “Yes, I double-checked that one too. All the sources agree. They must have to use lots of fertilisers to grow brassicas like that.” Down went the broccoli. Thankfully, I could replace it with kale – one of my favourite greens that happens to be low in GHG emissions as well. Excellent! I also decreased the cider intake, but thought I’d best leave in a pint or two for a sunny day.
With my GHG emissions now looking more ‘healthy’, I moved onto the next big issue: my energy (kilocalorie) intake was too high. And here is where I got stuck. I tried a few things: I replaced all my portion sizes with small ones, and cut out the chocolate and chips. I thought I’d be onto a winner. Not so. Next I ditched the second slice of toast for breakfast and the afternoon snack. Still no luck. I looked at the resulting overall weekly diet I’d ended up with: significantly reduced, yet still tasty and varied. The rest of my health indicators looked fine – it was a pretty rounded diet. In terms of micronutrients, I had to swap a couple of doses of peanut butter and jam for ‘yeast extract’ for breakfast to get my vitamin B12 up; and found out that I probably needed to eat a bit of seaweed every week to get some iodine without upping my salt intake too significantly, but everything else looked tickety-boo. I had a healthy diet. Apart from those kilocalories.
“I don’t know what to do Laura,” I said. “Unless I start cutting out whole meals – which I am fundamentally against! – I can’t see where I can make any more reductions, and I’m still eating too much.” When I’d told friends this result, they had suggested, encouragingly, that perhaps it was okay because I was a fairly active person and so maybe I needed the extra energy. “This is true,” Laura said “if you are physically active, you may require more in terms of energy than what is recommended in Laura’s Larder”. I do cycle to and from work (most days), but it is only a couple of miles. The recommendations, Laura explained, are based on a sedentary lifestyle (office job, driving to work etc), so I could have a little bit of wiggle room here, but I wasn’t convinced I did enough to get out of this one that easily.
Laura had a quick skim over my ‘model’ diet. “It looks like you eat pretty well!” she said, knowing I’d already made modifications. We went through it together and tried an experiment: first we took out the fry-up, and replaced it with a more normal breakfast. Tick! Kilocalorie intake all good. Then we put the fry-up back in, but took out the sunday lunch, and replaced it with some dahl and rice. Tick! Kilocalorie intake all good. In fact, if I took out either of these meals, I could add a few more things back into my diet – brie on toast for breakfast once a week (yum!), extra glass of wine here and there (fantastic!) and still eat a diet that was healthy, low in GHG emissions and (I thought) pretty tasty looking. Success!
Although I know I won’t be following the diet I ended up with to the letter (there’s no way I’m that organised!), there are a few good things I have already started doing: eating only either a fry-up or a sunday roast, generally eating less for each meal, re-thinking when I pick up some broccoli at the market, drinking less cider (thankfully, the sun doesn’t shine too much in Wales anyway), and having ‘yeast extract’ on my toast a couple more times a week. Now, I just need to find a way to sneak some seaweed into my weekly diet… Perhaps I can hide it in a stew? I’ll ask Mikhael, our excellent chef in the CAT restaurant.
Why not also read about the implications of what we eat on GHG emissions and land use, in our new report – People, Plate and Planet; also launched today.
Ranyl Rhydwen, a lecturer in CAT’s Graduate school of the Environment on the MSc Sustainability and Adaptation in the Built Environment, drills into the science of sea level rises and looks into the future. First posted by Sustain Magazine:
Humanity has already introduced enough CO2 into the atmosphere to raise the earth’s temperature by 4-6°C. This heat is being added at a rate approximately 300 times faster than when the earth’s ice sheets previously melted; past melt rates are therefore likely to provide low and conservative projections for the future. The earth’s remaining ice sheets contain 70 metres of sea level rise; with 40 metres of that being land locked in the East Antarctic Ice sheet that won’t melt unless CO2 reaches levels of >1000ppm. However the remaining 30m from Greenland, Western Antarctic Ice Sheet and the below sea level EAIS have all previously melted away when CO2 concentration levels were only 400-425ppm (April 2014 level 400ppm). A 30 metre sea level rise involves 50% of humanity, nearly all the world’s mega cities and large swathes of prime agricultural land. Sea levels will take thousands of years to fully rise, however 20 metres is inevitable and 30 metres probable. This needs planning for now as any manmade barrier is very unlikely to be able to cope with a 5 metre rise.
How fast will the melt occur?
Melt rates of up to 4 metres per century have previously occurred and although it is felt it would take the collapse of a major ice sheet to induce this 4 metre rate again, 1-2 metres per century is common, making the IPCC 80 cm projection by 2100 misguided considering the stakes involved. The 4m melt pulses occur due to the collapse of the marine based ice sheets. These ice sheets melt slowly at first as the glaciers get snagged on ocean bed ridges but once free of these ridges, they suddenly (after 200-1000 years) collapse in a process called rapid irreversible marine instability. These ice sheets are particularly vulnerable as they are melted from below by warm deep ocean waters lubricating the glacial flow and due to ocean dynamics warm waters (~3.5°C) currently bathe most of Greenland’s and Antarctica’s marine outlet glaciers.
The discovery that the Amundsen Sea outlet sea glaciers (that drain a third of the WAIS equivalent to 1.2 metres of sea level rise) have developed marine instability (i.e. they will now completely melt away) and are melting at an accelerating rate (30% greater than just 5 years ago) makes 4 metres a century look much more probable. Models suggest that this collapse is irreversible but may take 200-1000 years, however they didn’t account for the inevitable further warming of the melting waters. The last time Greenland, WAIS and parts of EAIS melted (120,000 years ago) melt rates of approximately 2 metres sea level rise per century occurred. The recent finding that the marine based glaciers draining the North East of Greenland (16% of it) have suddenly started rapidly melting and that the Fjords draining Greenland are much wider and extend further inland than previously thought all means that 4 metres in a century is again more likely. Therefore the recent evidence suggests that although 30 metres is the final outcome it is unlikely to occur by 2100, however 1-2 metres is virtually certain, 4-5 metres probable and greater amounts can’t be excluded.
Thus a large proportion of humanity is under direct threat from this sea level rise. The USA military are planning tactical retreat, however moving an army base is not moving a city (London), a state (Florida) or a country (Bangladesh). The first step in adapting to sea level rise is to slow it down and reduce its magnitude and the only way to do that is to remove (bio-sequester) carbon from the atmosphere and getting to 350ppm still means a 20-25 metre sea level rise and require a massive increase in mitigation efforts, which will take a transformation of societal systems to achieve. Adaptation and mitigation therefore need to be considered together. Adapting to sea level rise will mean more than building a sea wall as concrete barriers will have large carbon costs and will be overtopped eventually putting future generations at greater risk.
It seems we need to think again and take the approach of planned retreat, combined with innovative developments that embed humanity’s community into the new ecosystems and create new settlements that are robust to the extreme weather whilst sequestering carbon into the materials used to create them. That radical approach will take a transformation scale of change and the widespread uptake of progressive adaptation planning and is why here at Centre for Alternative Technology, we are putting transformational adaptation into the heart of our sustainability learning and teachings to help understand how to creatively approach the task that sea level rise imposes.