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. 2015 Nov 6;350(6261):aad0210.
doi: 10.1126/science.aad0210.

MAVEN observations of the response of Mars to an interplanetary coronal mass ejection

B M Jakosky  1 J M Grebowsky  2 J G Luhmann  3 J Connerney  2 F Eparvier  4 R Ergun  4 J Halekas  5 D Larson  3 P Mahaffy  2 J McFadden  3 D F Mitchell  3 N Schneider  4 R Zurek  6 S Bougher  7 D Brain  4 Y J Ma  8 C Mazelle  9 L Andersson  4 D Andrews  10 D Baird  11 D Baker  4 J M Bell  12 M Benna  2 M Chaffin  4 P Chamberlin  2 Y-Y Chaufray  13 J Clarke  14 G Collinson  2 M Combi  7 F Crary  4 T Cravens  15 M Crismani  4 S Curry  3 D Curtis  3 J Deighan  4 G Delory  3 R Dewey  4 G DiBraccio  2 C Dong  7 Y Dong  4 P Dunn  3 M Elrod  2 S England  3 A Eriksson  10 J Espley  2 S Evans  16 X Fang  4 M Fillingim  3 K Fortier  4 C M Fowler  4 J Fox  17 H Gröller  18 S Guzewich  2 T Hara  3 Y Harada  3 G Holsclaw  4 S K Jain  4 R Jolitz  3 F Leblanc  13 C O Lee  3 Y Lee  7 F Lefevre  13 R Lillis  3 R Livi  3 D Lo  18 M Mayyasi  14 W McClintock  4 T McEnulty  4 R Modolo  13 F Montmessin  13 M Morooka  4 A Nagy  7 K Olsen  7 W Peterson  4 A Rahmati  15 S Ruhunusiri  5 C T Russell  8 S Sakai  15 J-A Sauvaud  9 K Seki  19 M Steckiewicz  9 M Stevens  20 A I F Stewart  4 A Stiepen  4 S Stone  18 V Tenishev  7 E Thiemann  4 R Tolson  21 D Toublanc  9 M Vogt  14 T Weber  4 P Withers  14 T Woods  4 R Yelle  18
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MAVEN observations of the response of Mars to an interplanetary coronal mass ejection

B M Jakosky et al. Science. .

Abstract

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 solar wind during an interplanetary coronal mass ejection impact in March 2015. Responses include changes in the bow shock and magnetosheath, formation of widespread diffuse aurora, and enhancement of pick-up ions. Observations and models both show an enhancement in escape rate of ions to space during the event. Ion loss during solar events early in Mars history may have been a major contributor to the long-term evolution of the Mars atmosphere.

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