Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

23
Assessing Climate Changes in Arctic Sweden and Repercussions on Sami Reindeer Husbandry and Culture: Using a MODIS Image Time Series and Key Informant Interviews Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao The University of North Carolina at Chapel Hill Department of Geography

description

Assessing Climate Changes in Arctic Sweden and Repercussions on Sami Reindeer Husbandry and Culture: Using a MODIS Image Time Series and Key Informant Interviews. Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao The University of North Carolina at Chapel Hill - PowerPoint PPT Presentation

Transcript of Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Page 1: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Assessing Climate Changes in Arctic Sweden and Repercussions on Sami Reindeer Husbandry and Culture:

Using a MODIS Image Time Series and Key Informant Interviews

Gregory N. TaffThe University of Memphis

Department of Earth Sciences

Yang ShaoThe University of North Carolina at Chapel Hill

Department of Geography

Page 2: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Research Goals

1. Assess recent climate changes in Northern Sweden (current study 2000 – 2006)

2. Understand how climate changes impact and could impact Sami reindeer husbandry and Sami culture

3. Future work: develop new methods for stakeholders to use GIS to help manage land sustainably in this region

Page 3: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Climate Change in Fennoscandia Høgda et. al (2007)*

• Study area – all of Fennoscandia, 1982 – 1999 • AVHRR• Climate change assessed through changes in

growing season using NDVI– Growing season was determined for each pixel by

first calculating a mean NDVI (for NDVI>0) over the past 18 years. Growing season was defined to begin and end as the NDVI for the pixel passed this threshold (the mean).

• This method was found to correlate well with pollen and climate data indicating growing season

* Høgda, K., Karlsen, S., Tømmervik, H., “5 Changes in growing season in Fennoscandia 1982-1999”, in Arctic Alpine Ecosystems and People in a Changing Environment, Springer Berlin Heidelberg, pp. 71 – 84, 2007.

Page 4: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Change in Onset of Spring, 1982 - 1999Høgda et al. (2007)

Fig. Change in onset of spring during the period 1982 to 1999. Position of the pollen stations (star), phenological observation points (circle), and climatic stations (cross) used in Høgda et al. study.

Page 5: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Fig. Change in onset of autumn during the period 1982 to 1999.

Change in Onset of Autumn, 1982 - 1999Høgda et al. (2007)

Page 6: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Methods

• Remote sensing 2000 – 2006– Monitor annual landcover changes – MODIS vegetation cover (NDVI):

16-day composite (MOD13Q) product (v 5.0).• Date of first permanent snow cover• Date of snow melt • Date of peak NDVI • Peak NDVI• Average annual NDVI

– Future work: • Conduct analyses back in time using AVHRR to get longer coverage• Analyze climate data

• Key Informant Interviews– In what ways have Swedish Sami reindeer herders noticed local

climate changes?– How has climate change impacted and how might climate change

impact Sami reindeer husbandry?

Page 7: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

MODIS Specifications

Band No. Resolution (m) Bandwidth (um) SNR

1 250 620-670 1282 250 841-876 201

3 500 459-479 2434 500 545-565 2285 500 1230-1250 746 500 1628-1652 2757 500 2105-2155 110

8 1000 405-420 8809 1000 438-448 83810 1000 483-493 80211 1000 526-536 75412 1000 546-556 75013 1000 662-672 91014 1000 673-683 108715 1000 743-753 58616 1000 862-877 516

Band No. Resolution (m) Bandwidth (um) SNR

16 1000 862-877 516

(red)(NIR)

NDVI = (NIR - red) / (NIR + red)

Page 8: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Image Processing 1

• Water bodies and permanent snow cover masked out (pixels with negative NDVI throughout summer)

• For snow cover date calculations (snow cover determined by negative NDVI):– Date of first permanent snow cover:

• First date when at least 75% of study area is covered in snow (and remains covered for the winter)

– Date of snow melt:• First date when less than 75% of study area is covered in

snow

Page 9: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Image Processing 2

• Monitoring vegetation changes over time– All negative NDVI values deleted– Calculations for Peak NDVI for each year:

• For each image date, all nonnegative NDVI values were averaged

• Date of peak average NDVI determined for each year• Peak average NDVI recorded

– Calculations for annual Average NDVI:• For each year, an average was taken of all

nonnegative NDVI values of all dates in the year

Page 10: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Study Area

• All remote sensing analyses were conducted for:

1. Entire study area (Northern and North Central Sweden, east of high mountains)

2. Intensive Study Area (ISA) in North of Sweden (land around Övre Soppero)

• Future work: study area to be defined by extent of specific Sami village lands

– Large tracts of land where the reindeer herds owned by members of one “village” use throughout the year

– Some “villages” extend into Norway.

Page 11: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao
Page 12: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Results

Page 13: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

NDVI values averaged for the entire year (Northern Sweden)

Page 14: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Peak NDVI Value for each year (Norhtern Sweden)

Page 15: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Julian Days at NDVI peak values (Northern Sweden)

June 1

July 1

August 1

Page 16: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Year Snow melt Snow Cover

2000 129 321

2001 129 321

2002 129 321

2003 49 321

2004 129 321

2005 129 321

2006 97 321

Snow melt/cover for Northern Sweden

Page 17: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

NDVI values averaged for the entire year (ISA)

Page 18: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Peak NDVI Value for each year (ISA)

Page 19: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Julian Days at NDVI peak values (ISA)

Juli

an

day

June 1

July 1

August 1

Page 20: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Snow melt/cover for ISA

Year Snow melt Snow Cover

2000 129 321

2001 113 321

2002 129 321

2003 49 321

2004 129 321

2005 145 321

2006 97 321

Page 21: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Conclusions from remote sensing

• Average annual NDVI increasing for – Large Sweden study area– ISA in north of Sweden– Shows a likely general warming trend, continuing the trend of

elongated growing season shown by Høgda et al. (2007)

• Date of first snow cover very consistent over time• Peak NDVI values, date of peak NDVI, date of snow melt

– No clear trend– Not enough years of data (7 years)– Trends should be apparent when AVHRR data is processed

Page 22: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Significance of climate change on reindeer herding

• Lichen availability: video– Future work: monitor changes in lands

containing lichens– Grazing lands already in danger

• Mining • Forestry• Tourism structures

• Insects

• Layers of ice

Page 23: Gregory N. Taff The University of Memphis Department of Earth Sciences Yang Shao

Sami Culture• Cultural history and reindeer husbandry as far back as 7000 years• Reindeer husbandry

– Gives Sami rights to use land according to state governments– 10% of Sami herd reindeer

• Small percentage now rely solely on reindeer husbandry for income– Annual reindeer herding events maintain communities/families,

language and culture• Reindeer calving – spring• Ear marking – summer • Reindeer corralling - autumn

– Source of pride• World heritage

– Approx. 20,000 Sami– Potentially dying language and culture

• Sami culture historically oppressed by Scandinavian countries– Since late 20th century, a revival of Sami cultureh– Some schools now taught in Sami language

• Sami parliament – GIS mapping to show compromised Sami lands