s. e. stammerjohn , m. r. drinkwater, r. c. smith, and x. liu presented by brad goodwin
DESCRIPTION
Ice-atmosphere interactions during sea-ice advance and retreat in the Western Antarctic Peninsula region. S. E. Stammerjohn , M. R. Drinkwater, R. C. Smith, and X. Liu Presented by Brad Goodwin Atmospheric Science Graduate Student. Sea-Ice. Forms when surface temperature drops below 29° F - PowerPoint PPT PresentationTRANSCRIPT
Ice-atmosphere interactions during sea-ice advance and retreat in the
Western Antarctic Peninsula regionS. E. Stammerjohn, M. R. Drinkwater,
R. C. Smith, and X. LiuPresented by Brad Goodwin
Atmospheric Science Graduate Student
Sea-IceForms when surface
temperature drops below 29° FSalt excluded from ice, but still
saltier than land iceSea water becomes saltier and
denser, important for circulationTypically 1-6 feet thick around
AntarcticaChanges albedo and acts as an
insulator between ocean and atmosphere
Sea-Ice DynamicsChanges in position of
ice front with timeAtmospheric dynamics
or thermodynamics?How do ice-atmosphere
interactions respond to large scale atmospheric circulation patterns?
Western Antarctic PeninsulaCold, dry
continental air to the south
Warm, moist maritime air to the north
Data and MethodsUse satellite data and track extent as well as
motion of sea iceMeteorological data from two stations as well
as NCEP/NCAR Reanalysis dataDetermine opening, closing, and flux through
gatesDo not take into account tidal motion (short
time scale), only integrated 24-hour motion
Sea-Ice Extent
Sea-Ice Extent
Two Events – 1990 and 19921990 – Late onset
of sea-ice advance and late onset of sea-ice retreat
1992 – Early onset of sea-ice advance and early onset of sea-ice retreat
Four Days of Sea-Ice DriftFour consecutive days of
sea level pressure, wind, and sea ice drift
Red arrows added to show predominant direction of sea ice drift
Rapid changes in drift direction with changes in wind direction and speed
Also important for amount of open water detected
Comparison with Station DataCold temperatures, light
winds during sea-ice advance
Warm temperatures, strong northerly winds during sea-ice retreat
Largest day-to-day changes in extent and concentration were related to wind-driven sea-ice drift so…
The answer is…
Timing of Advance and RetreatJuly 1990 – northerly
winds, CPT near ice-edge, ice-edge retreats
August 1990 – CPT south of ice-edge, zonal winds, ice-edge recovers
July 1992 – high pressure, southerly winds, ice-edge advances
August 1992 – CPT near ice-edge, ice-edge retreats
TeleconnectionsSea-ice west of the Antarctic Peninsula behaves
differently than sea-ice in the rest of the southern hemisphere
Position and strength of CPT important for determining timing and extent of ice-edge advance and retreat
CPT influenced by the semi-annual oscillation (SAO) and El Nino-Southern Oscillation (ENSO)
SAO is a twice a year contraction and expansion of the pressure trough around Antarctica
Tropical Pacific is important for understanding sea-ice dynamics around Antarctica
Summary and ConclusionsAtmospheric dynamics drive
sea-ice edge anomaliesAnnual cycle in sea-ice edge is
determined by the persistence and intensity of regional atmospheric circulation
Changes in ice-edge over time are related to the amplitude and phase of the SAO (meridional temperature gradient) as influenced by ENSO and/or regional/global warming
Future DirectionsNeed to better understand teleconnection
relationships between the tropical Pacific and the Antarctic Peninsula region
My research focuses on an ice core collected from the Antarctic Peninsula
Evidence for relationship between accumulation on the AP and the Southern Annular Mode as well as ENSO
Teleconnections related to sea-ice dynamics and accumulation may have similar sources
These relationships need to be better understood