نتایج جستجو برای: solar atmosphere

تعداد نتایج: 169582  

2013
Marina Poje Branko Vuković Maja Varga Pajtler Vanja Radolić Igor Miklavčić Josip Planinić

The Earth is continually exposed to the cosmic radiation of both solar and galactic origin. Solar eruption and solar activity may affect cosmic radiation flux density which has a secondary effect on the flux of particles in the atmosphere as well. Such one event was recorded in the last week of October 2003, where the measured dose rate of the cosmic radiation in the aircraft ATR 42 was 1.8 tim...

Journal: :CoRR 2014
Andrew Leonard Huw Morgan

The solar atmosphere is a hot (~1MK), magnetised plasma of great interest to physicists. There have been many previous studies of the temperature of the Sun’s atmosphere ([Plowman2012], [Wit2012], [Hannah2012], [Aschwanden2013], etc.). Almost all of these studies use the SolarSoft software package written in the commercial Interactive Data Language (IDL), which has been the standard language fo...

Journal: :Journal of Physics: Conference Series 2010

Journal: :Journal of Physical Studies 2012

2007
WALTER ORR ROBERTS HAROLD ZIRIN

A number of significant recent advances in solar physics are reviewed. New kinds of observations made during the present sunspot cycle, which began in 1954, have emphasized still further the apparent complexity of solar phenomena and the need of nonequilibrium theoretical treatments. Among the new developments di cussed are solar cosmic rays and highenergy particles, flares and prominences, cor...

Journal: :Journal of Physical Studies 2013

Journal: :Journal of Physics: Conference Series 2008

Solar magnetic tornadoes are known to be one of the mass and energy transport mechanisms from the lower solar atmosphere into the upper layers of the solar corona. A bright spiral structure with two arms is observed using high-cadence EUV images of 171, 193 and 304 Ǻ channels of Atmospheric Imaging Assembly (AIA) aboard the Solar Dynamics Observatory (SDO) on 10th of July 2011 for three hours. ...

Journal: :Science 2015
B M Jakosky J M Grebowsky J G Luhmann J Connerney F Eparvier R Ergun J Halekas D Larson P Mahaffy J McFadden D F Mitchell N Schneider R Zurek S Bougher D Brain Y J Ma C Mazelle L Andersson D Andrews D Baird D Baker J M Bell M Benna M Chaffin P Chamberlin Y-Y Chaufray J Clarke G Collinson M Combi F Crary T Cravens M Crismani S Curry D Curtis J Deighan G Delory R Dewey G DiBraccio C Dong Y Dong P Dunn M Elrod S England A Eriksson J Espley S Evans X Fang M Fillingim K Fortier C M Fowler J Fox H Gröller S Guzewich T Hara Y Harada G Holsclaw S K Jain R Jolitz F Leblanc C O Lee Y Lee F Lefevre R Lillis R Livi D Lo M Mayyasi W McClintock T McEnulty R Modolo F Montmessin M Morooka A Nagy K Olsen W Peterson A Rahmati S Ruhunusiri C T Russell S Sakai J-A Sauvaud K Seki M Steckiewicz M Stevens A I F Stewart A Stiepen S Stone V Tenishev E Thiemann R Tolson D Toublanc M Vogt T Weber P Withers T Woods R Yelle

Coupling between the lower and upper atmosphere, combined with loss of gas from the upper atmosphere to space, likely contributed to the thin, cold, dry atmosphere of modern Mars. To help understand ongoing ion loss to space, the Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft made comprehensive measurements of the Mars upper atmosphere, ionosphere, and interactions with the Sun and s...

2013
Colin Goldblatt Tyler D. Robinson Kevin J. Zahnle David Crisp

The atmospheres of terrestrial planets are expected to be in long-term radiation balance: an increase in the absorption of solar radiation warms the surface and troposphere, which leads to a matching increase in the emission of thermal radiation. Warming a wet planet such as Earth would make the atmosphere moist and optically thick such that only thermal radiation emitted from the upper troposp...

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