Abstract
Snow precipitation is the primary mass input to the Antarctic ice sheet and is one of the most direct climatic indicators, with important implications for paleoclimatic reconstruction from ice cores. Provenance of precipitation and the dynamic conditions that force these precipitation events at four deep ice core sites (Dome C, Law Dome, Talos Dome, and Taylor Dome) in East Antarctica were analysed with air mass back trajectories calculated using the Lagrangian model and the mean composite data for precipitation, geopotential height and wind speed field data from the European Centre for Medium Range Weather Forecast from 1980 to 2001. On an annual basis, back trajectories showed that the Atlantic-Indian and Ross-Pacific Oceans were the main provenances of precipitation in Wilkes Land (80%) and Victoria Land (40%), respectively, whereas the greatest influence of the ice sheet was on the interior near the Vostok site (80%) and in the Southwest Ross Sea (50%), an effect that decreased towards the coast and along the Antarctic slope. Victoria Land received snowfall atypically with respect to other Antarctica areas in terms of pathway (eastern instead of western), seasonality (summer instead of winter) and velocity (old air age). Geopotential height patterns at 500 hPa at low (>10 days) and high (2–6 days) frequencies during snowfall cycles at two core sites showed large positive anomalies at low frequencies developing in the Tasman Sea-Eastern Indian Ocean at higher latitudes (60–70°S) than normal. This could be considered part of an atmospheric blocking event, with transient eddies acting to decelerate westerlies in a split region area and accelerate the flow on the flanks of the low-frequency positive anomalies.
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Acknowledgments
This research was carried out as part of the framework of the Project on Glaciology of the PNRA-MIUR, and was financially supported by the PNRA Consortium through a collaboration with ENEA Roma. The Talos Dome Ice core Project (TALDICE), a joint European programme, is funded by national contributions from Italy, France, Germany, Switzerland and the United Kingdom. Primary logistical support was provided by PNRA at Talos Dome. This is TALDICE publication no 10. We acknowledge the ice2sea project, funded by the European Commission’s 7th Framework Programme through grant number 226375, ice2sea manuscript number 15.
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Appendix 1: acronyms
Appendix 1: acronyms
- AAO:
-
Antarctic Oscillation
- AN:
-
Antarctica Sector
- ATL:
-
Atlantic Ocean Sector
- CPT:
-
CircumPolar Trough
- DC:
-
Dome C
- DdU:
-
Dumont D’Urville
- ECMWF:
-
European Centre Medium Range Weather Forecast
- EPICA:
-
European Project for Ice Coring in Antarctica
- ERA:
-
European Re-Analysis
- FLEXPART:
-
Lagrangian Particle Dispersion Model
- HYSPLIT:
-
Hybrid Single-Particle Lagrangian Integrated Trajectory
- IND:
-
Indian Ocean Sector
- LWD:
-
Law Dome
- NOAA:
-
National Oceanic and Atmospheric Administration
- PO:
-
Pacific Ocean Sector
- PSA:
-
Pacific South American
- RS:
-
Ross Sea Sector
- TALDICE:
-
TAlos Dome Ice CorE
- TDN:
-
Talos Dome
- TLD:
-
Taylor Dome
- VSK:
-
Vostok
- E u :
-
Eliassen-Palm flux vector
- f:
-
Coriolis parameter
- GP :
-
Geopotential fields
- GP ANOM :
-
Anomaly in GP field with respect to the long term annual mean
- RH w :
-
Relative Humidity with respect to water
- SF:
-
Precipitation
- T :
-
Temperature
- u :
-
Zonal wind component
- v :
-
Meridional wind component
- w :
-
Vertical wind component
- ϕ :
-
Latitude
- σ :
-
Static stability
- CL:
-
Cluster group
- \( CL_{IND1}^{TDN} \) :
-
Cluster for TJ starting from TDN and coming from high latitude over the Indian Ocean Sector
- \( CL_{IND2}^{TDN} \) :
-
Cluster for TJ starting from TDN and coming from low latitude over the Indian Ocean Sector
- \( CL_{ROSS}^{TDN} \) :
-
Cluster for TJ starting from TDN and coming from the Ross Sea Sector
- \( CL_{PAC}^{TDN} \) :
-
Cluster for TJ starting from TDN and coming from the Pacific Ocean Sector
- \( CL_{IND}^{DC} \) :
-
Cluster for TJ starting from DC and coming from the Indian Ocean Sector
- \( CL_{PAC}^{DC} \) :
-
Cluster for TJ starting from DC and coming from the Pacific Ocean Sector
- \( CL_{IND1}^{LWD} \) :
-
Cluster for TJ starting from LWD and coming from high latitude over the Indian Ocean Sector
- \( CL_{IND2}^{LWD} \) :
-
Cluster for TJ starting from LWD and coming from low latitude over the Indian Ocean Sector
- \( CL_{ROSS}^{TLD} \) :
-
Cluster for TJ starting from TLD and coming from the Ross Sea Sector
- \( CL_{PAC}^{TLD} \) :
-
Cluster for TJ starting from TLD and coming from the Pacific Ocean Sector
- MPts :
-
Map time series
- MPts GP :
-
Map time series for Geopotential field
- \( MPts_{{}}^{{E_{u} }} \) :
-
Map time series for E-P flux vector
- \( MPts_{{}}^{{\nabla \cdot E_{u} }} \) :
-
Map time series for E-P flux vector divergence
- TJ:
-
Back Trajectory
- TMR:
-
Blocking index as defined in Tibaldi et al. (1995)
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Scarchilli, C., Frezzotti, M. & Ruti, P.M. Snow precipitation at four ice core sites in East Antarctica: provenance, seasonality and blocking factors. Clim Dyn 37, 2107–2125 (2011). https://doi.org/10.1007/s00382-010-0946-4
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DOI: https://doi.org/10.1007/s00382-010-0946-4