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CECS Glacier Research
Andrés Rivera and the CECs team
Laboratorio de Glaciología y Cambio Climático Centro de Estudios Científicos (CECS), Valdivia
Who we are? SENIOR RESEARCHERS
Gino Casassa Andrés Rivera
ASSOCIATED RESEARCHERS Robert Thomas, NASA Wallops Flight Facility, USA
Eric Rignot, JPL-NASA, USA Norbert Blindow, BGR
POST-DOCTORAL FELLOWS Marious Schaefer
Anja Wendt ASSISTANT RESEARCHERS (present and formers)
Daniela Carrión (Geographer) Francisca Bown (Geographer MSc)
Sebastián Cisternas (Computer Engineer) Juan Andrés Uribe (Electronic Engineer) Rodrigo Zamora (Electronic Engineer)
Thomas Loriaux (MSc) Claudio Bravo (presently at UCH)
Pablo Zenteno (presently in a private company) RESIDENT OFFICERS
Max Fuentealba, Chilean Air Force UNDERGRADUATES STUDENTS
Many ¡¡¡¡¡
Our key issues We would like to
Define a Chilean glacier base line
Study remote and “virgin” areas
Apply airborne, ground and oceanographic geophysical methods
Develop new technologies for glacier research
Improve our capacity building effort
Provide information for decision makers
Trying to answer the following questions: How are the glaciers responding to climatic changes?
Are all glaciers good indicators of climate change?
What are the consequences of recent glacier behaviour for our population and economic activities?
What are the consequences of human activities on glacier behaviour?
Could be possible to model glacier dynamics and the consequences of the glacier responses?
Main problems for glaciological research in Chile
Scarce and poor availability of field data
Lack of regular and accurate glacier cartography
Limited budgets for software/hardware/data/training/monitoring
Inefficient and bureaucratic data distribution among national institutions
Reduced collaboration between scientists and institutions
Few systematic monitoring programs
Few specialists and trained people
State of art in Chile Almost complete but out of date glacier inventory
Frontal, areal and ice elevation changes have been analysed for
hundred of glaciers combining historical records, remotely sensed imagery and field data
Preliminary satellite image data base
GIS data base for restricted number of glaciers including surface topography, frontal variations, available imagery
Several glaciological methods have been applied; Remote sensing, GPS, LIDAR, RES (ground, airborne, helicopter borne), Fixed cameras, AWS’s, Sonars, ice coring, modelling, runoff.
Only two mass balance programmes
Some statistics
•Postgraduate people in glaciology: <10
•Pre-post degrees in glaciology: 0
•Institutions doing glacier research: <10
•Number of glaciology related grants funded in Chile in recent years: <15 (of 9979)
0
20
40
60
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1950 1960 1970 1980 1990 2000
DÉCADAS
N° P
UBL
ICAC
ION
ES
Number of publicaciones per decade
Hydro-meteorological stations for glacier studies
0 10 20 30 40 50 60 70 80 90 100 110 12002468
1012141618202224262830
Distancia mínima a una fuente glaciar [km]
Núm
ero
de e
stac
ione
s
0 1000 2000 3000 4000 5000 60000
2
4
6
8
10
12
14
16
18
20
Diferencia de elevación estacion-glaciar [m]
Few stations with long records
Previous CECs studies Glacier inventory
Northern and Southern Patagonian icefields Aconcagua basin Cordillera Darwin, Mte Sarmiento, isla Santa Inés, isla Hoste Nevados de Payachatas Several ice-capped volcanoes in southern Chile
Frontal, areal and volumetric changes Almost 150 studied glaciers all around the country
Mass and energy balance In 2003, CECS initiated a systematic program on Glaciar Mocho at Volcán Mocho, in the Chilean lake District. Geodetic mass balance estimations in several glaciers There is one glacier where a mass balance model has been applied Several AWS´s installed on top of glaciers in central-southern Chile in combination with met data analysis and
cameras Applied geophysics
LIDAR of more than 40 glaciers. RES (ground and airborne) of more than 50 glaciers Sonar/calving studies of more than 5 glaciers Ice velocities in more than 5 glaciers (GPS, feature tracking cameras) Ice volcanic interactions using thermal cameras in 3 volcanoes
Glacio-chemistry Several short ice cores and snow samples for biological and chemical studies Deep ice cores in 5 glaciers in combination with institutions from abroad (Switzerland, Japan, etc.)
First glacier inventory south of the Estrecho de Magallanes: 3289km2
Isla Santa Inés: 274 km2
Monte Sarmiento: 273 km2
Cordillera Darwin: 2333 km2
Isla Hoste: 409 km2
Fuente: CECS, 2008
A mountain glacier (Alpine?) Glaciar Universidad
(National Estrategy, DGA)
Field data collection and preliminary models:
-0,8
-0,6
-0,4
-0,2
0
0,2
0,4
0,6
0 800 1600 2400 3200
Nº Registro
Dife
renc
ia (m
)
8 Mayo 200928 Marzo 2009
-5
0
5
10
15
20
0 800 1600 2400 3200
Nº de Registro
Tem
pera
tura
(ºC
)
28 Marzo 2009 8 Mayo 2009
Ablation
Temperatures
AWS at accumulation and ablation zones
0
0,2
0,4
0,6
0,8
1
1000 1200 1400 1600 1800 2000 2200 2400 2600 2800 3000
mm
eq.
a.
Modelled versus measured ablation
Records 0
200
400
600
800
1000
1200
Dates
Glo
bal R
adia
tion
(W m
-2)
Global radiation
Stations
Hydrological station affected by the March 11, 2010 Earthquake
-7
-6
-5
-4
-3
-2
-1
0
1
2
2400 2500 2600 2700 2800 2900 3000 3100 3200 3300 3400Altitud SRTM (m s.n.m.)
Cam
bios
de
elev
ació
n (m
/a)
1955/20092000/2009
Elevation changes at Glaciar Universidad (m/a)
A calving glacier
Ice velocities from fixed cameras (m/d)
7 - 10 10 - 14 14 - 17 17 - 24
Ice-capped volcanoes:Monitoring Volcán Villarrica
Thermal studies Perfil Nocturno
píxel
0 50 100 150 200 250 300
TºC
100
200
300
400
500
600
700
800
Temperatura v/s pixel
Volcán Villarrica, Mayo 13, 2010
Volcán Chaitén
Mass balance studies: Volcán Mocho
Accumulation (a), ablation (b) y mass balance (c) in m w. eq. a-1
(a) (c) (b)
2003/2004
2004/2005
(a) (b) (c)
-0.88
+0.36
LIDAR and THERMAL surveys: Volcán Hudson 7 - 10 10 - 14 14 - 17 17 - 24
Some methods everywhere: Ice thickness
Foto: Andrés Rivera Radar surveys (5 MHz)
Airborne radar test
Helicopterborne radar
Helicopter borne radar survey in Central Chile
A B
A B
Juncal Sur Glacier
CECS and BGR from Germany
CAMS-1: Cecs Airborne Mapping System
Lago desaparecido: CECS-Armada 2007
CAMS profile versus SRTM
0
20
40
60
80
100
120
140
160
180
200
0
1000
2000
3000
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7000
8000
9000
1000
0
1100
0
1200
0
1300
0
1400
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1500
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1600
0
1700
0
1800
0
1900
0
Distance (m)
Alti
tude
(m a
e)
Outwash Plain Missing Lake
Outwash Plain Lake Ice
Ice
Lake Ice
Missing Lake
Lake Valley Lake River
SRTM 2000
CECS 2007
Sea LevelIce
LakeMoraine
Moraine
A A’
A
A’
Glaciar Témpanos
Glaciar Bernardo
1975-2000 -4.7± 0.8 -3.6 ± 0.8
2000-2007 -4.9 ± 3.0 -8.1 ± 3.0
The siphon..
GLOF events
October 10, 2008 Photos: Andrés Rivera
Ice core from Pio XI glacier
Detail Glacier Monitoring Programme
(DGMP)
Northern Chile (CEAZA?) - Glaciar Tapado - Location: 30°08’S
Central Chile (DGA-ACQWA-CECS-UCH?)
- Glaciares Juncal Norte, Echaurren-Olivares -Universidad - Location: 33°-34°’S -
Lake District (CECS) - Glaciares Chillán-Villarrica and Mocho - Location: 39°S
Field Instrumentation - AWS - Gauge stations - Stake network - Photogrammetric cameras
Ground and airborne survey - GPR and GPS - Airborne and terrestrial Laser scanning -Aerial photogrammetry -Thermal and normal cameras
Aisén (DGA-CECS) - Glaciar San rafael-Colonia - Nef- Jorge Montt Location: 46-48°S
Magallanes -Glaciar Pio XI (CECS) -Glaciar Grey (UMAG) -GCP (Trier U.)
Monitoring network implementation
Future tasks CECs will hold an ACCION workshop in Valdivia
In May 2012 we will have technical meeting (CECS-DGA) with USGS and
colleagues from VTI for testing GASS.
In August 2012 we will have a training course in collaboration with the US Embassy and the USGS (GASS). The idea is having a few days in Valdivia and then going to Volcán Mocho with colleagues from other institutions in Chile.
Both workshops may be together or one after the other.
Looking for new students
Searching for Postdocs (mainly from abroad) interested in doing research in our countries
Conclusions and recommendations Most of our glaciers are retreating fast, however not everything is related to
Climate change¡¡¡¡ In Chile there are many “anomalies”.
What is an anomaly? Each glacier has particular settings, and no one is an easy one (Alpine?)
We don’t have enough trained people to do research in the country
We have a lot of requests from the government, private companies and the academia, but we are too few and with limited time for everything
Budget is also a restriction, especially when bureaucrats are taking control of some funding agencies
We don’t have people doing glacier modelling
Modelling is very restrict due to the lack of data for many regions. We need to improve our glaciological base line.
Thanks
CECS, FONDECYT, Fundación Andes, GLIMS, USGS, UCH, ICM, NASA, USA Embassy.