Deriving CME volume and density from remote sensing data
<p>Using combined STEREO-SOHO white-light data, we present a method to determine the&#160;volume and density of a coronal mass ejection (CME) by applying the graduated cylindrical&#160;shell model (GCS) and deprojected mass derivation. Under the assumption that the CME &#160;mass is roughly equally distributed within a specific volume, we expand the CME self-similarly and calculate the CME density for distances close to the Sun (15&#8211;30 Rs) and at 1 AU.&#160;The procedure is applied on a sample of 29 well-observed CMEs and compared to their&#160;interplanetary counterparts (ICMEs). Specific trends are derived comparing calculated and&#160;in-situ measured proton densities at 1 AU, though large uncertainties are revealed due to&#160;the unknown mass and geometry evolution: i) a moderate correlation for the magnetic&#160;structure having a mass that stays rather constant and ii) a weak&#160;correlation for the sheath density by assuming the sheath region is an extra mass&#160;- as expected for a mass pile-up process - that is in its amount comparable to the initial CME&#160;deprojected mass. High correlations are derived between in-situ measured sheath density&#160;and the solar wind density and solar wind speed as measured 24&#160;hours ahead of the arrival of the disturbance. This gives additional confirmation that the&#160;sheath-plasma indeed stems from piled-up solar wind material. While the CME&#160;interplanetary propagation speed is not related to the sheath density, the size of the CME&#160;may play some role in how much material is piled up.</p>