welcome to the peak district national park. moorlands as indicators of climate change initiative...
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Moorlands as Indicators of Climate Change InitiativeMoorlands as Indicators of Climate Change Initiative
Welcome to MICCI
This is a project designed for schools to investigate the interrelationship between the moorland
landscape and climate change
Chris Robinson Learning and Discovery Officer PDNPA
High Open Countryside
No normal farming
Created by humans
So What is ‘Moorland’?So What is ‘Moorland’?
Moorland EcologyMoorland Ecology
Characteristics and Types
HEIGHT: >250m above sea level
SOIL: Peat up to 4m thick
Vegetation
Peat
Gritstone bedrock
WINDY & WET: >1000mm/year
All types have impoverished flora
Harsh physical conditions
Poor soil structure and nutrient status
1. Heather moorland - most common, on gentler, relatively dry slopes
2. Grass moorland - coarse grasses such as mat grass, wet areas, peat <20cm allowing grass roots to penetrate
3. Cotton grass moorland - rare, wet areas, peat >70cm
4. Sphagnum bog - formerly 18 species, but pollution has reduced these to 3, of which only 1 is common. Very wet and acid. An absorbent, spongy mass. Note that 13% of world’s blanket bog is in UK
“The warming of the climate is unequivocal”IPCC report 2007(Intergovernmental Panel on Climate Change)
Climate Change – it’s definitely happening!Climate Change – it’s definitely happening!
Where do moorlands fit into the climate change debateWhere do moorlands fit into the climate change debate??
1. Peatlands are the single largest carbon reserve in the UK (3 billion tonnes of carbon) More carbon is stored in UK peat than in the forests of the UK and France combined.
2. A good peat bog actively “sequesters” carbon (locks it away) . Is a “CARBON SINK”
3. A damaged peat bog actively loses carbon to the atmosphere.(through erosion and oxidation).
Is a “CARBON SOURCE”
4. The warmer and drier the climate is the more erosion and fires there are. The more carbon turns into CO2.
Peat
Weathering of bedrock
Rain
Photosynthesis
Decomposition
Dissolved Inorganic Carbon DIC
Particulate Organic Carbon POC
Dissolved Organic Carbon DOC
CO2 INPUTS CO2 OUTPUTS
The Moorland Carbon CycleThe Moorland Carbon Cycle
Fluvial Flux (removed by water)
A healthy moorA healthy moor
Carbon flux prediction models (Dark Peak area)
Best case scenario Worst case scenario
= Carbon loss
= Carbon sink
Source: Sea-viewing Wide Field-of-View Sensor
(SeaWiFS) Project, NASA-GSFC, and ORBIMAGE,
18 April 2003
Fire on Bleaklow
Satellite view of Northern Britain
Fire can turn a healthy moor into an unhealthy one!
Aerial view of fire damage and subsequent erosion on Bleaklow
It’s not all bad though!
The Moors for the Future partnership have managed
to reseed this area of erosion on Sykes Moor and many others
Large areaof bare peat
Total length of soil spikeSoil depth – soil spikeSoil temperature - thermometer
length of soil spike above ground
Holes to let water inMeasure this!
Dip well for gauging water table
1 metre
5 cm
Metre rule
Kitchen waste pipeSurface of Peat
Holes to let water inMeasure this!
Quadrats Heather Bilberry Crowberry
1 lll lllll ll
2 ll l
3 l
4 l l
5 l
2 different plants, 2 tally marks1 plant, 1 tally mark
Who else is involved?Who else is involved?Carlton High
Honley High
Longley Park
King Ecgberts
St John HoughtonHeanorgateLong Eaton
West Hill
Glossopdale
Chapel High
Painsley Catholic College
What sort of conservation work will our experiments inform?What sort of conservation work will our experiments inform?
Youth Rangers using Geojute fabric to stabilise planting
Discoveries you make about the state of the peat will helpscientists from Moors for the Future decide on the most appropriate conservation methods for the moorland.