- What are the most important themes you have learned?
This week I learned more about the Anthropocene, a term I first heard a few weeks ago in one of the Adaptation to climate change seminar series. I learned that the Earliest evidence of anthropogenic impact included prehistoric flint workings at Grime's Graves at around 3000-2000 BC.
Also calculated my individual carbon footprint as 2.51 tonnes (Home, 0.61 tonnes; Appliances 1.74 tonnes; Travel 0.16 tonnes) which was less than I anticipated.
The course has reinforced what I have learned about climate change from other sources. Probably the most important theme is ocean acidification, something I knew little about - What aspect(s) did you find difficult?
Nothing this week caused me much difficulty.
Again, I found nothing during the course that was really difficult. I don't find writing particularly easy but I found that using blogger was relatively straightforward. Might even encourage me to blog on other topics. - What did you find most interesting? And why?
Both this week and throughout the course I have found the presentation of the course material excellent! Perhaps most interesting were the weekly feedback sessions which were similar to university tutorials. I also enjoyed reading and participating in the discussions with other students. - Was there something that you learned that prompted you to do your own research?
I am very interested in the Arctic and was prompted to look at Observational determination of albedo decrease caused by vanishing Arctic sea ice after I heard it mentioned in a seminar I attended. I also looked at Calving on tidewater glaciers amplified by submarine frontal melting.
I contacted Anglia Ruskin University regarding the building I used as an example and received a useful reply from them. - Are there any web sites or other online resource that you found
particularly useful in furthering your knowledge and understanding?
I keep an eye on the National Snow & Ice Data Center to follow the progress of the Arctic Death Spiral.
I had the good fortune to attend the seminar series mentioned above. The materials from the seminars are available here.
Saturday, 8 March 2014
Week 8 Reflection
Friday, 28 February 2014
Week 7 Reflection
Really interesting week. As someone who has had a low energy renovation on my home I was particularly interested in the buildings chosen for their design by fellow students. I spent ages going through the discussion entries for that section. There were plenty I would like to visit but that would not be good for my carbon footprint!
One that I particularly liked was the Chilterns Gateway Centre suggested by Greg Baker. That one should be near enough to visit.
I only saw the Channel4 "Restoration Man" programme episode on Thrum Mill by chance. Very impressive what can be done with a relatively modest amount of money and huge amounts of effort and dedication! Always good to see such an interesting building given a new lease of life.
Attended the last of the Adaptation to climate change seminar series by Professor Charlie Kennel. You may listen to Prof Kennel's lectures and access the teaching material here. This last seminar summarised the earlier seminars and went on to discuss how “Knowledge Action Networks” comprising international experts and local decision‐makers can foster informed and timely decisions at the regional and local levels. I feel extremely privileged living in Cambridge where I am able to attend such seminars at no cost and even have a free drink or two afterwards with some very interesting and distinguished audience members.
This week's major frustration was not being able to present my photographs of my building design example on a map using geotags. I took the pictures, manually added approximate geotags to the pictures using geotag, set up a flickr account, uploaded the pictures but still couldn't get it to use the geotags embedded in the EXIF to do anything useful! I did finally get a map created with a single geotag for all eleven pictures.
One that I particularly liked was the Chilterns Gateway Centre suggested by Greg Baker. That one should be near enough to visit.
I only saw the Channel4 "Restoration Man" programme episode on Thrum Mill by chance. Very impressive what can be done with a relatively modest amount of money and huge amounts of effort and dedication! Always good to see such an interesting building given a new lease of life.
Attended the last of the Adaptation to climate change seminar series by Professor Charlie Kennel. You may listen to Prof Kennel's lectures and access the teaching material here. This last seminar summarised the earlier seminars and went on to discuss how “Knowledge Action Networks” comprising international experts and local decision‐makers can foster informed and timely decisions at the regional and local levels. I feel extremely privileged living in Cambridge where I am able to attend such seminars at no cost and even have a free drink or two afterwards with some very interesting and distinguished audience members.
This week's major frustration was not being able to present my photographs of my building design example on a map using geotags. I took the pictures, manually added approximate geotags to the pictures using geotag, set up a flickr account, uploaded the pictures but still couldn't get it to use the geotags embedded in the EXIF to do anything useful! I did finally get a map created with a single geotag for all eleven pictures.
Tuesday, 25 February 2014
Week 7 - Building design near you
My choice of building and urban landscape near me is Anglia Ruskin University, Young Street, Cambridge, just a short distance along New Street from my house. Phase 1 is almost ready for use and I have had the opportunity to see the site developed.
There are two parts to the current stage of the development: the newly built Health Building; and a Victorian primary school, known as the Ragged School, which has been renovated to form the Music Therapy Centre.
Features of note on the Health Building are the chimney-like structures which act as (passive?) ventilation stacks; the smaller, non-opening, windows on the north side to reduce heat loss and limit road noise from New Street; the brise soleil (louvres) on the south side to reduce direct sunlight but still take full advantage of natural light; and, just about visible, solar photovoltaic panels on the roof angled to improve energy collection.
Note that the brise soleil only cover the upper part of the south side of the Health Building. The next phase will be another building that will shade the lower part.
The Music Therapy Centre is an excellent example of the renovation of an older building. Many of the original external features have been retained. New double-glazing is in keeping with the style of the building and there appears to be secondary glazing on some windows which should improve both thermal and acoustic performance. The stepped entrance has been replaced with an access-friendly ramp and handrails.
I think that heating of both buildings is by gas. There is a large gas main entering The Ragged School and I have seen exhaust or condensate coming from the nearest of the stacks to my house which has an extra dimple on top.
There is no car parking on site but there is parking for around 250 bicycles. Staff and students will be expected to use walking, bikes or public transport.
One tiny criticism is that there are lights set at pavement level shining vertically up through the outside 'V' of each od the pair of ventilation stacks. This seems an unnecessary waste of energy and a source of light pollution.
Even though I took all my pictures from public space around the building I received attention from a member of Anglia Ruskin University security staff! I explained that it was for a personal project but he didn't seem convinced. Take care when taking pictures.
There are two parts to the current stage of the development: the newly built Health Building; and a Victorian primary school, known as the Ragged School, which has been renovated to form the Music Therapy Centre.
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| Health Building from New Street |
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| Health Building from New Street |
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| Health Building from St. Matthew's Street |
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| Health Building from Young Street |
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| Music Therapy Centre from Young Street |
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| Music Therapy Centre from Young Street |
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| Solar PV just visible over the roof of Brunswick Nursery School |
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| Close up of brise soleil on south side of Health Building |
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| Dormer window and roof lights on Music Therapy Centre |
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| Long shot from outside my front door |
Note that the brise soleil only cover the upper part of the south side of the Health Building. The next phase will be another building that will shade the lower part.
The Music Therapy Centre is an excellent example of the renovation of an older building. Many of the original external features have been retained. New double-glazing is in keeping with the style of the building and there appears to be secondary glazing on some windows which should improve both thermal and acoustic performance. The stepped entrance has been replaced with an access-friendly ramp and handrails.
I think that heating of both buildings is by gas. There is a large gas main entering The Ragged School and I have seen exhaust or condensate coming from the nearest of the stacks to my house which has an extra dimple on top.
There is no car parking on site but there is parking for around 250 bicycles. Staff and students will be expected to use walking, bikes or public transport.
One tiny criticism is that there are lights set at pavement level shining vertically up through the outside 'V' of each od the pair of ventilation stacks. This seems an unnecessary waste of energy and a source of light pollution.
Even though I took all my pictures from public space around the building I received attention from a member of Anglia Ruskin University security staff! I explained that it was for a personal project but he didn't seem convinced. Take care when taking pictures.
Friday, 21 February 2014
Week 6 Reflection
Interesting to learn that some fungal species are moving to the higher latitudes at around three kilometres per year. Can't help wondering what happens to fungal species that are specific to particular trees? Fungal spores can move large distances on the wind but it takes a lot longer for trees to move into a new area and grow to maturity.
Who is to speak for the unloved or unknown fungi? Perhaps we need the fungal equivalent of the Ugly Animal Preservation Society?
Attended the penultimate seminar of the Adaptation to climate change seminar series entitled California and the Arctic. Professor Peter Wadhams was in the audience which lead to a very interesting questions and answers session at the end of the seminar.
Of particular interest was a just published paper, Observational determination of albedo decrease caused by vanishing Arctic sea ice. It reports that albedo decrease caused by vanishing Arctic sea ice [was] considerably larger than expectations from models and recent less direct estimates. Averaged globally, this albedo change is equivalent to 25% of the direct forcing from carbon dioxide during the past 30 years. Also learnt that the US Navy has detailed mapping data of Arctic sea ice thickness which was collected to identify suitable missile launch areas!
Interesting to contrast the problems of drought, wild fires, and water shortages in California with the flooding in the UK. It was surprising to learn that the Hoover Dam which creates Lake Mead, the largest reservoir in the United States in maximum water capacity, could within a few years drop to the point where it could not generate electricity.
Who is to speak for the unloved or unknown fungi? Perhaps we need the fungal equivalent of the Ugly Animal Preservation Society?
Attended the penultimate seminar of the Adaptation to climate change seminar series entitled California and the Arctic. Professor Peter Wadhams was in the audience which lead to a very interesting questions and answers session at the end of the seminar.
Of particular interest was a just published paper, Observational determination of albedo decrease caused by vanishing Arctic sea ice. It reports that albedo decrease caused by vanishing Arctic sea ice [was] considerably larger than expectations from models and recent less direct estimates. Averaged globally, this albedo change is equivalent to 25% of the direct forcing from carbon dioxide during the past 30 years. Also learnt that the US Navy has detailed mapping data of Arctic sea ice thickness which was collected to identify suitable missile launch areas!
Interesting to contrast the problems of drought, wild fires, and water shortages in California with the flooding in the UK. It was surprising to learn that the Hoover Dam which creates Lake Mead, the largest reservoir in the United States in maximum water capacity, could within a few years drop to the point where it could not generate electricity.
Friday, 14 February 2014
Week 5 Reflection
I learnt more about the mechanisms behind ocean acidification. It would have been useful if I had studied more chemistry!
It's always good to see the Devon seaside in the fine summer weather. I have many happy memories of family holidays at my grandmother's in Honiton and visits to places like Exmouth, Budleigh Salterton, Sidmouth, Beer and Lyme Regis. I studied at Exeter University and it's been fun trying to spot places I remember in the background like the arboretum.
Attended the latest in the Adaption to climate change seminar series on Thursday evening entitled Sea Level Rise, Coastal Cities, and Wetlands. It was useful when thinking about the questions about sea level rise in this week's session. Professor Charlie Kennel is a very interesting speaker and I think there are plans to use the seminar series as the basis of a MOOC. The Centre for Science and Policy exists to promoting engagement between researchers and policy professionals. Unfortunately, speaking to other attendees over drinks afterwards I think all of them were from a science background. The politicians and policy professionals who really need to understand about climate change didn't appear to be there.
Back in the 1970s I worked for the Water Data Unit, part of the Department of the Environment. While there I worked with Terry Marsh, one of the authors of The Recent Storms and Floods in the UK (February 2014). I am very sad and disappointed at the poor treatment of the professionals at the Environment Agency as reported in Floods: Environment Agency frontline staff hit by cuts, whistleblowers reveal.
It's very disappointing that many politicians and media commentators seem unaware of resources such as the Science Media Centre and and their briefings on Expert reaction to continued flooding.
It's always good to see the Devon seaside in the fine summer weather. I have many happy memories of family holidays at my grandmother's in Honiton and visits to places like Exmouth, Budleigh Salterton, Sidmouth, Beer and Lyme Regis. I studied at Exeter University and it's been fun trying to spot places I remember in the background like the arboretum.
Attended the latest in the Adaption to climate change seminar series on Thursday evening entitled Sea Level Rise, Coastal Cities, and Wetlands. It was useful when thinking about the questions about sea level rise in this week's session. Professor Charlie Kennel is a very interesting speaker and I think there are plans to use the seminar series as the basis of a MOOC. The Centre for Science and Policy exists to promoting engagement between researchers and policy professionals. Unfortunately, speaking to other attendees over drinks afterwards I think all of them were from a science background. The politicians and policy professionals who really need to understand about climate change didn't appear to be there.
Back in the 1970s I worked for the Water Data Unit, part of the Department of the Environment. While there I worked with Terry Marsh, one of the authors of The Recent Storms and Floods in the UK (February 2014). I am very sad and disappointed at the poor treatment of the professionals at the Environment Agency as reported in Floods: Environment Agency frontline staff hit by cuts, whistleblowers reveal.
It's very disappointing that many politicians and media commentators seem unaware of resources such as the Science Media Centre and and their briefings on Expert reaction to continued flooding.
Week 5 - The impact of ocean acidification
Will marine organisms be able to adapt to ocean acidification given the time scale for the predicted changes?
Adaptation to changing conditions is by evolution where those most able to withstand the changes will tend to survive. This takes many generations so organisms with short life cycles (bacteria and other micro organisms) can adapt faster than longer lived organisms such as fish and mammals.
The rapid pace of ocean acidification may mean that some organisms go extinct because they cannot adapt quickly enough.
Not all organisms are equally affected by ocean acidification. Those without shells or similar structures requiring calcium may not be directly affected. Others might even benefit from greater acidity or the lack of competition from those affected.
The changes may be felt throughout the food chain as changes in prey populations affect their predators.
The marine environment is already under threat from other man-made problems such as overfishing and pollution including plastics. Ocean acidification is another driver towards mass extinctions.
I think it was a talk I attended by The Black Fish UK where the audience was asked about major marine predators. Apparently, one of them is the domestic chicken as they are largely fed on fishmeal!
For more information on plastic pollution see Plastic Soup Foundation and Beat the Microbead.
Increased carbon dioxide in the atmosphere is likely to lead to sea level rise. Are rising sea levels more of a threat to humanity than ocean acidification?
Very difficult to decide. Both will have negative effects but the sections of the humanity affected may be different.
Those in low lying developing countries such as the Pacific island nations, India, Pakistan, Bangladesh, Vietnam, Egypt and others will be the first to feel the effects of sea level rise. Even in the developed countries most of the population lives within 100 km of the coast, many of them in cities. Some of the wealthy cities (New York, London, Venice) may be able to build expensive flood prevention schemes but even these may only delay the inevitable flooding from major sea level rises. Flooding, especially, salt water inundation, will be a threat to land grown food production.
We depend on the survival of some marine organisms which take in carbon dioxide and produce oxygen. Anything that damages this process will have an effect on the atmosphere and may result in a further increase in greenhouse gases. Many coastal communities depend on the sea for their food and changes in the marine environment may reduce that food supply.
Adaptation to changing conditions is by evolution where those most able to withstand the changes will tend to survive. This takes many generations so organisms with short life cycles (bacteria and other micro organisms) can adapt faster than longer lived organisms such as fish and mammals.
The rapid pace of ocean acidification may mean that some organisms go extinct because they cannot adapt quickly enough.
Not all organisms are equally affected by ocean acidification. Those without shells or similar structures requiring calcium may not be directly affected. Others might even benefit from greater acidity or the lack of competition from those affected.
The changes may be felt throughout the food chain as changes in prey populations affect their predators.
The marine environment is already under threat from other man-made problems such as overfishing and pollution including plastics. Ocean acidification is another driver towards mass extinctions.
I think it was a talk I attended by The Black Fish UK where the audience was asked about major marine predators. Apparently, one of them is the domestic chicken as they are largely fed on fishmeal!
For more information on plastic pollution see Plastic Soup Foundation and Beat the Microbead.
Increased carbon dioxide in the atmosphere is likely to lead to sea level rise. Are rising sea levels more of a threat to humanity than ocean acidification?
Very difficult to decide. Both will have negative effects but the sections of the humanity affected may be different.
Those in low lying developing countries such as the Pacific island nations, India, Pakistan, Bangladesh, Vietnam, Egypt and others will be the first to feel the effects of sea level rise. Even in the developed countries most of the population lives within 100 km of the coast, many of them in cities. Some of the wealthy cities (New York, London, Venice) may be able to build expensive flood prevention schemes but even these may only delay the inevitable flooding from major sea level rises. Flooding, especially, salt water inundation, will be a threat to land grown food production.
We depend on the survival of some marine organisms which take in carbon dioxide and produce oxygen. Anything that damages this process will have an effect on the atmosphere and may result in a further increase in greenhouse gases. Many coastal communities depend on the sea for their food and changes in the marine environment may reduce that food supply.
Thursday, 13 February 2014
Week 5 - Calving events
I remember watching the largest glacier calving ever filmed in Chasing Ice. There is a clip from The Guardian that identifies it as the Ilulissat glacier although it appears to be the Jakobshavn Isbræ. It is an excellent film as is Thin Ice.
The recent paper by M. O’Leary and P. Christoffersen, Calving on tidewater glaciers amplified by submarine frontal melting, they use a finite-element model of stresses near the front of a tidewater glacier to investigate the effects of frontal melting on calving. They refer to earlier modelling studies which focused largely on the effects of basal and surface melting.
Solar and atmospheric warming are likely to increase surface melting. Melt water that reaches the base of the glacier will increase melting there and by increasing lubrication increase the speed of the glacier. This will cause calving to increase.
Increasing sea water temperature could increase undercutting of the ice front due to frontal melting considerably increasing the calving rate.
As the glacier calving front retreats the fjord topography may change which could also affect calving rate if the length of the calving front changes.
My thoughts are that the key controlling processes are basal, frontal and surface melting and that the length of the calving front will also have an impact.
The recent paper by M. O’Leary and P. Christoffersen, Calving on tidewater glaciers amplified by submarine frontal melting, they use a finite-element model of stresses near the front of a tidewater glacier to investigate the effects of frontal melting on calving. They refer to earlier modelling studies which focused largely on the effects of basal and surface melting.
Solar and atmospheric warming are likely to increase surface melting. Melt water that reaches the base of the glacier will increase melting there and by increasing lubrication increase the speed of the glacier. This will cause calving to increase.
Increasing sea water temperature could increase undercutting of the ice front due to frontal melting considerably increasing the calving rate.
As the glacier calving front retreats the fjord topography may change which could also affect calving rate if the length of the calving front changes.
My thoughts are that the key controlling processes are basal, frontal and surface melting and that the length of the calving front will also have an impact.
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