PALMER, ANTARCTICA Long Term Ecological Research PAL Summer Cruise LMG 05-01 04 - 31 Jan, 2004.
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Transcript of PALMER, ANTARCTICA Long Term Ecological Research PAL Summer Cruise LMG 05-01 04 - 31 Jan, 2004.
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PALMER, ANTARCTICALongTermEcological Research
PAL Summer CruiseLMG 05-0104 - 31 Jan, 2004
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Palmer Station – Nov 22, 2004 PALMER, ANTARCTICA Long Term Ecological Research
Program (LTER)
• Part of US LTER Network of 26 sites
• 1991 – present, 14 January cruises
• Regional (200,000 km2) and local sampling
• Focus on sea ice dynamics, water column processes and apex predators
• Physics, remote sensing and ice, microbial biogeochemistry, sedimentation, primary production, krill, penguins
Aerial photo of Anvers Island and Gerlache Strait courtesy Chilean Navy
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Eight Principal investigators:
Hugh Ducklow (VIMS): microbial biogeochemistryRobin Ross & Langdon Quetin (UCSB): krillRay Smith (UCSB): bio-optics & remote sensingMaria Vernet (Scripps): phytoplanktonBill Fraser (Polar Res Inst): penguinsDoug Martinson (LDEO): physical oceanographyKaren Baker (Scripps): information management & outreach
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DESERT ECOLOGY
Sevilleta LTER SiteBlack Grama grassland
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The central tenet of PAL is that the annual advance and retreat of sea ice is a major physical determinant of spatial and temporal changes in the structure and function of the Antarctic marine ecosystem…We now recognize the west Antarctic Peninsula (WAP) as a premier example of a climate-sensitive region experiencing major changes in species abundance and composition due to changes in range and distribution that are occurring in response to regional climate change manifested here primarily as a southern migration of principal climate characteristics (climate migration). In effect, the maritime system of the northern WAP is replacing the continental, polar system of the southern WAP along the peninsular climate gradient. This change is driven by regional warming, which is modulated by regional hydrography, sea ice processes and global teleconnections to lower latitude atmospheric variability…we seek to understand the full ecological implications of climate migration in the WAP, and uncover the mechanisms linking them through teleconnections to global climate variability.
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What we know:
Regional warming (+5C in winter; +2C annual) over past 5 decadesSea ice extent, duration decliningThese two highly correlated; mechanisms are beginning to beunderstood.
Interannual variability in sea ice behavior
Penguins declining locally (70% since 1975): but mechanisms and links to climate not clear…some factors may be terrestrial (e.g., snow).
What we think:
Some relationship between sea ice variability and plankton dynamics:
High ice years High PP (eg, 1996) Low ice low PP (eg, 1999)But krill optimize on ‘average ice years’ ??? And no real highs, lows in the 1990s…
Links between lower trophic levels and penguins also unclear
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Palmer temperature, 1975 - 2002 !
Year
1975 1980 1985 1990 1995 2000
degrees Celsius
-5
-4
-3
-2
-1
0regressionr2 = 0.28p < 0.02
No data 1982, 87-89
1980s: Hi/Lo temps1990s: Not
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Palmer annual mean ice extent, 1979 - 2003
Year
1980 1985 1990 1995 2000
103 kilometers
20
40
60
80
100
120
140
160
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Palmer sea ice & temperature, 1979 - 2001
degrees Celsius
-5 -4 -3 -2 -1 0
103 kilometers
60
80
100
120
140
160
r2 = 0.75p < 0.001***
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SEA ICE EXTENTarea of coverage
in sampling grid
Solid lines: coverage for current yearDotted lines: 1990-99 mean
Black: total extentBlue: open water within ice packRed: Difference
Data courtesy S. Stammerjohn LDEO
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Palmer Adelie population, 1973 - 2002
Year
1975 1980 1985 1990 1995 2000
Breeding pairs
4000
6000
8000
10000
12000
14000
16000
18000
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SeaWIFS Chlorophyll, January 1998 - 2003
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Primary Production
1990 1992 1994 1996 1998 2000 2002 2004
PP gC m
-2 yr
-1
0
100
200
300
400
PP mgC m
-2 d-1
0
200
400
600
800
1000
1200
1400
Palmer PPGrid PP
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WAP 1996 Carbon Solution
gpS = Gross PP forSmall Phytoplankton
gpL = Gross PP forLarge Phytoplankton
bac = bacteriadet = detritus
ext = Export
kri = krill
mic = microzooplankton
pro = protozoans
pen = penguins
myc = myctophids
doc = dissolved organic matter
Krill grazing of Large
Phytoplankton is 42 % of PP.
Largest flows are Krill grazing and respiration. Upper Trophic level flows are very small.
Penguin consumption of krill equal to 0.1 % of PP.
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WAP 1999 Carbon SolutiongpS = Gross PP forSmall Phytoplankton
gpL = Gross PP forLarge Phytoplankton
bac = bacteriadet = detritus
ext = Export
kri = krill
mic = microzooplankton
pro = protozoans
pen = penguins
myc = myctophids
doc = dissolved organic mattersal = salps
Krill grazing of Large
Phytoplankton is 21 % of PP.
Total Salp ingestion is 21 % of PP.
Salps have significant role in food web.
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The Cruise…
1. The Grid2. Process Stations3. Sediment Trap4. “Inside” stations5. Rothera6. King Neptune
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RotheraRothera
Marguerite Bay
Trap mooring
Rothera &Avian Island
Renaud Island
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Nm
ol leu
cine l -1 h
r-1
Bacterial productionJanuary LMG cruise2003
Microbes & biogeochemistryPAL-LTER annual meeting 2003
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Sedimentation rate at 170 meters
YEAR1993 94 95 96 97 98 99 00 01 02 03 04
mgC m
-2 d-1
0
20
40
60
80
100
120
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Sea ice 11 Dec. 2004
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General structure of the cruise
Sample LTER Grid Stationstop-to-bottom CTD cast with 12 samples zooplankton towsrevisit Palmer Stations B, E 3 timesroutine, “core” measurements3-4 stations per day
Recover and redeploy Sediment Trap Mooring (15 Jan)
3 Process Stationsnorth, middle and south regions on gridca. 24 hours eachexperimental work and repeat sampling
Deploy birders Renaud Island (1 day) Avian Island (4 days)
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General structure of the cruise, continued
High resolution grid near Palmer StationCTD and netsaround 13 Janpersonnel swap (krill group)
Visit Rothera Station Saturday 22 Jan.Exchange personnelLocal CTD sampling & intercalibrationParty!Depart 0600 Sunday, resume operations
King Neptune visits vessel 01 Feb.
Caveats:Expect 2-3 days lost to stormsExpect to lose stations due to ice