منابع مشابه
Ice-core net snow accumulation and seasonal snow chemistry at a temperate-glacier site: Mount Waddington, southwest British Columbia, Canada
A 141m ice core was recovered from Combatant Col (51.3858N, 125.2588W; 3000ma.s.l.), Mount Waddington, Coast Mountains, British Columbia, Canada. Records of black carbon, dust, lead and water stable isotopes demonstrate that unambiguous seasonality is preserved throughout the core, despite summer surface snowmelt and temperate ice. High accumulation rates at the site (>4m ice eq. a) limit modif...
متن کاملAn ice-core record of net snow accumulation and seasonal snow chemistry at Mount Waddington, southwest British Columbia, Canada
A 141m-deep ice-core was retrieved from Combatant Col (51.39° N, 125.22° W, 3000m), Mount Waddington, Coast Mountains, British Columbia, Canada. Records of black carbon, dust, lead, and water stable-isotopes show that unambiguous seasonality is preserved throughout the core, despite summer surface snowmelt and temperate ice. High accumulation rates at the site (in excess of 5 m a) limit modific...
متن کاملPulsar observations at Mt . Pleasant
Two daily pulsar monitoring programs are progressing at the Mount Pleasant Observatory, Hobart, Tasmania, Australia. A new system involving the 26-metre radio telescope monitors 10 young pulsars daily and is focussed on near-real-time glitch finding. This will allow Target of Opportunity observations to measure post-glitch heating of the neutron star surface (Helfand, Gotthelf, & Halpern 2001)....
متن کاملTurbulence Monitoring at Mount John
In this paper we present preliminary results of a turbulence monitoring campaign at the Mount John University Observatory using a bread-board based SCIDAR (SCIntillation Detection And Ranging) system. Simultaneous SCIDAR and generalised SCIDAR data are captured and used to quantify the turbulence at the site. Initial results, including estimates of key turbulence parameters, are presented and d...
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ژورنال
عنوان ژورنال: Monthly Weather Review
سال: 1906
ISSN: 0027-0644,1520-0493
DOI: 10.1175/1520-0493(1906)34<326a:srampm>2.0.co;2