Recent Talks

El instrumento IMaX ha sido entregado al proyecto SUNRISE, un telescopio solar de 1 m de diámetro que volará este verano desde el polo norte en un globo LDB de NASA. En este coloquio veréis como ha sido el proceso de integración del instrumento español IMaX y cual es el status del proyecto SUNRISE que involucra a tres países: EEUU, Alemania y España con la participación del IAC, IAA (Granada), INTA (Madrid), GACE (Valencia) y la UPM (Madrid).

The magnetic landscape of the polar region (Tsuneta et al, 2008) is characterized by vertical kilogauss patches with super-equipartition field strength, a coherence in polarity, lifetimes of 5-15 hr, and ubiquitous weaker transient horizontal fields (Lites et al 2008, Ishikawa & Tsuneta, 2008, 2009). Polar region in 2007 have abundant vertical fields much stronger than the quiet Sun. Unipolar appearance and disappearance of the kG vertical patches must be closely related to properties of the horizontal flow field in the polar region. Difference and similarity between the quiet sun and the polar region are summarized, and its implication for solar dynamo will be discussed. All the open field lines forming the polar coronal hole essentially originate from such magnetic patches, and the fast solar wind would emanate from these vertical flux tubes seen in the photosphere. We conjecture that vertical flux tubes with large expansion around the photospheric-coronal boundary serve as efficient chimneys for Alfven waves that accelerate the solar wind. Indeed, we discovered propagating Alfven waves (kink mode) with magneto-acoustic waves (sausage mode) in the solar photosphere with period of 4-13 minutes with Hinode spectro-polarimeter (Fujimura and Tsuneta, 2009). We found that these fluctuations are superposition of ascending and descending Alfven waves with almost equal intensities from the analysis of the phase relationship between transverse magnetic and velocity fluctuations. Aflven waves along flux tubes in the quiet sun appear to be efficiently reflected back probably at photosphere-corona boundary. It would be very interesting to measure possible change in the reflectivity of Alfven waves depending on the magnetic environment.

Comets may have played an important role in depositing the organic matter that, between 4,6 and 3,6 billion of years ago, allowed the formation of life on the primordial Earth. Nowadays, many complex organic molecules are routinely observed in the gaseous component of the comae by radio and near-IR observations. However a large quantity of organic matter may be under the form of solid, either as organic grains or organics embedded in silicate grains. The Giotto mission to the 1P/Halley comet revealed for the first time the in-situ presence of organic grains, that accounted for almost 50% of the mass of organic matter in its coma. Remote detection of these organic grains in other comets is very difficult because they rapidly sublimate under the solar radiation and their spectroscopic signatures are hidden within those of the refractory cometary dust. In this talk I will give a short review on the organic matter in comets, I will describe a method for detecting organic grains in comets and I will present recent results.