Convective Snowfalls Linked to the Interaction of a Boundary-Layer Front with a Mesoscale Cyclone Near Terra Nova Bay, Antarctica

Author:

Bove Roberto,Paolo Grigioni

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Reference32 articles.

1. Adams AS, Tripoli GJ (2003) Use of the UW-NMS to simulate the flow around Ross Island on 3 September 2003. In: Antarctic Automatic Weather Station Annual Meeting, Antarctic Meteorological Research Center Annual Meeting, and Antarctic Mesoscale Prediction System (AMPS) Users’ Workshop. Joint Annual Meetings, Charleston, SC, 8–10 June 2004. Preprints. S.l., 2004, pp 20–22

2. Bromwich DH (1986) Boundary layer meteorology of the western Ross Sea. Antarct J 21(5): 237–240

3. Bromwich DH (1989a) Satellite analyses of Antarctic katabatic wind behavior. Bull Am Meteorol Soc 70: 738–749

4. Bromwich DH (1989b) An extraordinary katabatic wind regime at Terra Nova Bay. Antarct Mon Weather Rev 117: 688–695

5. Bromwich DH (1990) Organization of clouds and precipitations in extratropical cyclones. In: Newton CW, Holopainen EO (eds) Extratropical cyclones: the Erik Palmén Memorial volume. American Meteorological Society, Boston, MA, pp 129–153

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