cryosphere components in gtos networks

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Cryosphere components in GTOS networks Wilfried Haeberli Geography Department University of Zurich

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Cryosphere components in GTOS networks. Wilfried Haeberli Geography Department University of Zurich. Global Terrestrial Observing System GTOS cryosphere networks. sea ice (GOOS) GTN-G: glaciers GTN-P: permafrost GTN-S: snow GTN-IS: continental ice sheets. - PowerPoint PPT Presentation

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Page 1: Cryosphere components     in GTOS networks

Cryosphere components in GTOS

networks

Wilfried HaeberliGeography Department

University of Zurich

Page 2: Cryosphere components     in GTOS networks
Page 3: Cryosphere components     in GTOS networks

Global Terrestrial Observing System GTOScryosphere networks

sea ice (GOOS)

GTN-G: glaciers

GTN-P: permafrost

! GTN-S: snow

! GTN-IS: continental ice sheets

Page 4: Cryosphere components     in GTOS networks

Global Terrestrial Observing System GTOScryosphere networks

sea ice (GOOS)

GTN-G: glaciers

GTN-P: permafrost

! GTN-S: snow

! GTN-IS: continental ice sheets

Page 5: Cryosphere components     in GTOS networks

flow velocity 13 km/y

flow velocity 7 km/y

Jakobshavn Isbrae

Page 6: Cryosphere components     in GTOS networks

Ice shelves

• Canadian• Antarctica

1906 Ice Shelf Extent 1906 Ice Shelf Extent (~10,000 km(~10,000 km22))

Eureka

Copland

Page 7: Cryosphere components     in GTOS networks

Ice shelves

• Canadian• Antarctica

1906 Ice Shelf Extent 1906 Ice Shelf Extent (~10,000 km(~10,000 km22))

2008 Ice Shelf Extent 2008 Ice Shelf Extent (~1000 km(~1000 km22))

Eureka

Copland

Page 8: Cryosphere components     in GTOS networks

Global Terrestrial Observing System GTOScryosphere networks

sea ice (GOOS)

GTN-G: glaciers

GTN-P: permafrost

! GTN-S: snow

! GTN-IS: continental ice sheets

Page 9: Cryosphere components     in GTOS networks

Global Glacier Changes: facts and figures

Project management & editing:Michael Zemp, Jaap van Woerden

Scientific authors:Michael Zemp, Isabelle Roer, Andreas Kääb,Martin Hoelzle, Frank Paul, Wilfried Haeberli

Design, layout, maps & graphics:Diana Rizzolio

Page 10: Cryosphere components     in GTOS networks

monitoring principle:

integration of

in-situ measurements, remote sensing and numerical modelling

Page 11: Cryosphere components     in GTOS networks

time

base inventory

repeat inventory

repeat inventory

fluct

uatio

ns o

f gl

acie

rs

mass balance length change

area/volume/thickness change

spaceglacier inventories

mass balance length change

area/volume/thickness change

Page 12: Cryosphere components     in GTOS networks

UNEP press release 16.03.2008:

• new record loss: - 1.4 m w.e.

• average loss rate 1980-1999doubled since 2000

• previous record (1998) exceededin 2003, 2004, 2006

• only 1 positive balance (Echaurren)

WGMS 2008

Page 13: Cryosphere components     in GTOS networks

Zemp et al. (2007)

Page 14: Cryosphere components     in GTOS networks

Recession of Morteratsch Glacier, Switzerland, between 1985 and 2007.Source: J. Alean, SwissEduc (www.swisseduc.ch) / Glaciers online (www.glaciers-online.net).

2007

1985

Glacier length changes

Page 15: Cryosphere components     in GTOS networks

DEM-differencing: SRTM - DTM 25

Page 16: Cryosphere components     in GTOS networks

GlobGlacier

European Space Agency (ESA)GLIMS

Global Land Ice

Measurement from Space

Baffin Island

Paul

glacier inventories/satellite observations

Page 17: Cryosphere components     in GTOS networks

Glacier distribution around the world

Zemp et al. (2007), based on Dyurgerov and Meier (2005)

Page 18: Cryosphere components     in GTOS networks

Noetzli 2008

Ellesmere Island, Canadian Arctic

Page 19: Cryosphere components     in GTOS networks

UN Organisations

Page 20: Cryosphere components     in GTOS networks

annual report swiss offer gtn-g general assembly nc

Launch of GTN-G website

Page 21: Cryosphere components     in GTOS networks

New GTN-G meta-data browser

Data layers:

length change mass balance volume change special events glacier maps

WGI

GLIMS

glacier photograph collection

Interactive map interface showing FoG (brown dots), WGI (blue dots) and GLIMS (pink polygons) data

Page 22: Cryosphere components     in GTOS networks

General cryosphere:• Establishment of GTN-S (snow) and GTN-IS (continental ice sheets) has high

priority• how about ice shelves (sea ice/GTNG/GTN-IS) and outlet glaciers (GTN-

G/GTN-IS)?

GTN-G:Future strategy/Recommendations

• GTN-G operates with a well established, tiered/integrative monitoring strategy, which should continue and may serve as a model

for other GTNs;• Quality ranking should be introduced with respect to in-situ measurements

(especially glacier mass balance)• GTN-G representatives are involved in IPCC work and should formally be

consulted in the review process for future assessment reports

Questions/guidance/feedbacks from the GTOS SC• GTOS SC to agree with organisational structure and lead responsibility of

GTN-G as developed by the partner institutions (WGMS, NSIDC, GLIMS) and IACS/IUGG/ICSU• GTOS SC to transfer the overall responsibility for GTN-G to GTN-G Steering

CommitteeProposed actions to be endorsed by GTOS SC

• Agreements on institutional responsibilities and lead structure of IACS