Title: COASTAL ICE CORE RECORDS ON ENVIRONMENTAL CHANGES IN ANTARCTICA: RESULTS FROM INDIAN ITASE
1COASTAL ICE CORE RECORDS ON ENVIRONMENTAL CHANGES
IN ANTARCTICA RESULTS FROM INDIAN ITASE
-
- Thamban Meloth
- National Centre for Antarctic Ocean Research
- Ministry of Earth Sciences (Govt. of India)
- Vasco-da-Gama, GOA 403 804
Website www.ncaor.gov.in ltgt E-mail
meloth_at_ncaor.org
2Oceans Poles
Southern (water) hemisphere 91 water
coverage Antarctica 70 of worlds freshwater
Northern (land) hemisphere51 water coverage
http//oceancolor.gsfc.nasa.gov/cgi/biosphere_glob
es.pl
3Maitri (1989)
D.Gangotri (1983-90)
At Larsemann Hills 20xx
INDIA IN ANATARCTICA
4Poles are no longer poles apart!
One-to-one coupling of glacial climate
variability in Greenland and Antarctica (EPICA
Members, 2006)
5Ice core vs. Instrumental temperature data.
Influence of SAM on Antarctic temperature
(Schneider et al., 2006)
6 INDIAN INITIATIVES ITASE
Indian ITASE concentrates along a coastal to
inland transect in the central Dronning Maud Land
7-
- SCIENTIFIC QUESTIONS?
- How did the coastal Antarctic environment
respond to the changes in global climate as well
as to extreme events such as volcanic eruptions
during the past? - How did the climatic teleconnections
influenced the atmospheric chemistry of coastal
Antarctica as recorded in snow? - What are the spatial variations and its causes
within the temporal records from different
locations in Antarctica? - What was the role of external and/or internal
forcing mechanisms on the Antarctic environment? -
-
8 STUDY AREA
ANTARCTICA
Central Dronning Maud Land
Ingrid Christensen Coast
9RECENT FIELD CAMPAIGNS IN EAST ANTARCTICA
ICE CORE DRILLING coastal Dronning Maud Land
? IND-25/B5 Lat. 71 20.5 S Long. 11 35.6
E (25th InSEA) ? IND-26/B6 Lat. 70º 11.4 S
Long. 12º 27.1 E (26th InSEA) ? IND-26/B7
Lat 70º 13.8 S Long. 11º 55.7 E (26th InSEA)
SNOW SAMPLING Ingrid Christensen Coast ?
LARSEMANN TRANSECT ? PUBLICATIONS ICE SHELF
TRANSECT ? AMERY ICE SHELF TRANSECT
10FIELD ACTIVITIES 2006-07
11LABORATORY ACTIVITIES
12- Ice cores as archives of past volcanic events
Core IND-22/B4
Thamban et al., 2006 Curr. Science
13 Micro-particles in ice significance
Ice-melts were filtered in the CLASS 100 room
scanned using SEM-EDS.
Core IND-22/B4
Laluraj et al., 2008 ENV. MON. ASSESS
14 Microbial cells adhered to micro-tephra
Laluraj et al., 2008 ENV. MON. ASSESS
Core IND-22/B4
15- Solar forcing on Antarctic chemistry change?
Core IND-25/B5
16 High-resolution stable isotope studies
Core IND-25/B5
17 Relation between ice core ?18O El Niño ?
Naik et al., 2008 Gcubed- under review
Core IND-25/B5
18 Combined effect of ENSO AAO on ?18O
temperature?
Core IND-25/B5
Naik et al., 2008 Gcubed- under review
19 Snow accumulation rate ?18O
Core IND-25/B5
20 Deuterium excess Shift in moisture source
21SURFACE SNOW STUDIES ALONG INGRID CHRISTENSEN
COAST
22FRACTIONATION OF SULPHUR COMPONENTS IN SNOW
(nssSO42-) (SO42-) - 0.252 (Na)
Thamban et al., 2008, Under Review, Appl. Geochem.
23FROST FLOWER FORMATION FRACTIONATION
(nssSO42-) (SO42-) - 0.252 (Na)
Thamban et al., 2008, Under Review, Appl. Geochem.
24BIOLOGICAL CONTRIBUTION TO SNOW AEROSOL CHEMISTRY
(nssSO42-) (SO42-) - 0.252 (Na)
Antony et al., Under Review, GRL
Thamban et al., 2008
25SNOW BIOGEOCHEMISTRY CLIMATE LINKAGE
(nssSO42-) (SO42-) - 0.252 (Na)
Antony et al., Under Review, GRL
26- IMPORTANT FINDINGS
- Shallow ice cores from coastal Antarctica provide
light on the spatial and temporal variations in
the climate and environment. - Large volcanic events associated with anomalous
sulphate peaks also reveal presence of
micro-tephra. Some of these particles harbor
microbial cells adhered to surfaces, supporting a
significant micro-niche in accreted ice, hitherto
unknown. - High-resolution ice core studies in relation to
instrumental data also reveal that the coastal
Antarctic climate and snow accumulation is
influenced by the combined ENSO and AAO forcings.
- Coastal Ice core data is also seems to support
the influence of solar forcing on Antarctic
environment. - Surface snow samples from coastal region provide
vital clues on biogeochemical cycling of sulphur
and nitrogen and atmospheric budget.
27- FUTURE OUTLOOK
- The Indian program envisages increased activities
to obtain more cores under the ITASE program. - More efforts are also being made to obtain ice
cores that record 2000 years of climate/
environmental change. The 2K represent- Natural
(MWP) anthropogenic (20th Century) warming
important for climate modeling sub-annual
resolution possible - Asian collaboration is also warming up under the
aegis of Asian Forum on Polar Sciences (AFoPS -
China, India, Japan, Korea Malaysia). AFoPS may
conduct a collaborative shallow ice core project
in in Arctic too. - Increased collaboration in field and science with
ITASE partners?
28Thanks!