Search Publications

Chromospheric Alfvénic Waves Strong Enough to Power the Solar Wind
DOI: 10.1126/science.1151747 Bibcode: 2007Sci...318.1574D

Schrijver, C. J.; Ichimoto, K.; De Pontieu, B. +11 more

Alfvén waves have been invoked as a possible mechanism for the heating of the Sun's outer atmosphere, or corona, to millions of degrees and for the acceleration of the solar wind to hundreds of kilometers per second. However, Alfvén waves of sufficient strength have not been unambiguously observed in the solar atmosphere. We used images of high te…

2007 Science
Hinode 761
The Process of Tholin Formation in Titan’s Upper Atmosphere
DOI: 10.1126/science.1139727 Bibcode: 2007Sci...316..870W

Coates, A. J.; Young, D. T.; Waite, J. H. +4 more

Titan’s lower atmosphere has long been known to harbor organic aerosols (tholins) presumed to have been formed from simple molecules, such as methane and nitrogen (CH4 and N2). Up to now, it has been assumed that tholins were formed at altitudes of several hundred kilometers by processes as yet unobserved. Using measurements …

2007 Science
Cassini 501
Evidence for Alfvén Waves in Solar X-ray Jets
DOI: 10.1126/science.1147050 Bibcode: 2007Sci...318.1580C

Weber, M.; Golub, L.; Kano, R. +11 more

Coronal magnetic fields are dynamic, and field lines may misalign, reassemble, and release energy by means of magnetic reconnection. Giant releases may generate solar flares and coronal mass ejections and, on a smaller scale, produce x-ray jets. Hinode observations of polar coronal holes reveal that x-ray jets have two distinct velocities: one nea…

2007 Science
Hinode 398
Chromospheric Anemone Jets as Evidence of Ubiquitous Reconnection
DOI: 10.1126/science.1146708 Bibcode: 2007Sci...318.1591S

Matsumoto, Takuma; Shibata, Kazunari; Nishizuka, Naoto +19 more

The heating of the solar chromosphere and corona is a long-standing puzzle in solar physics. Hinode observations show the ubiquitous presence of chromospheric anemone jets outside sunspots in active regions. They are typically 3 to 7 arc seconds = 2000 to 5000 kilometers long and 0.2 to 0.4 arc second = 150 to 300 kilometers wide, and their veloci…

2007 Science
Hinode 374
Coronal Transverse Magnetohydrodynamic Waves in a Solar Prominence
DOI: 10.1126/science.1145447 Bibcode: 2007Sci...318.1577O

Lites, B. W.; Ichimoto, K.; Shibata, K. +10 more

Solar prominences are cool 104 kelvin plasma clouds supported in the surrounding 106 kelvin coronal plasma by as-yet-undetermined mechanisms. Observations from Hinode show fine-scale threadlike structures oscillating in the plane of the sky with periods of several minutes. We suggest that these represent Alfvén waves propagat…

2007 Science
Hinode 324
Subsurface Radar Sounding of the South Polar Layered Deposits of Mars
DOI: 10.1126/science.1139672 Bibcode: 2007Sci...316...92P

Gurnett, Donald A.; Stofan, Ellen R.; Frigeri, Alessandro +21 more

The ice-rich south polar layered deposits of Mars were probed with the Mars Advanced Radar for Subsurface and Ionospheric Sounding on the Mars Express orbiter. The radar signals penetrate deep into the deposits (more than 3.7 kilometers). For most of the area, a reflection is detected at a time delay that is consistent with an interface between th…

2007 Science
MEx 295
Tracking Solar Gravity Modes: The Dynamics of the Solar Core
DOI: 10.1126/science.1140598 Bibcode: 2007Sci...316.1591G

García, Rafael A.; Turck-Chièze, Sylvaine; Mathur, Savita +5 more

Solar gravity modes have been actively sought because they directly probe the solar core (below 0.2 solar radius), but they have not been conclusively detected in the Sun because of their small surface amplitudes. Using data from the Global Oscillation at Low Frequency instrument, we detected a periodic structure in agreement with the period separ…

2007 Science
SOHO 242
Martian Atmospheric Erosion Rates
DOI: 10.1126/science.1134358 Bibcode: 2007Sci...315..501B

Barabash, Stas; Lundin, Rickard; Fedorov, Andrei +1 more

Mars was once wet but is now dry, and the fate of its ancient carbon dioxide atmosphere is one of the biggest puzzles in martian planetology. We have measured the current loss rate due to the solar wind interaction for different species: Q(O+) = 1.6·1023 per second = 4 grams per second (g s-1), Q(O2

2007 Science
MEx 235
Continuous Plasma Outflows from the Edge of a Solar Active Region as a Possible Source of Solar Wind
DOI: 10.1126/science.1147292 Bibcode: 2007Sci...318.1585S

Golub, Leon; DeLuca, Edward E.; Harra, Louise K. +18 more

The Sun continuously expels a huge amount of ionized material into interplanetary space as the solar wind. Despite its influence on the heliospheric environment, the origin of the solar wind has yet to be well identified. In this paper, we report Hinode X-ray Telescope observations of a solar active region. At the edge of the active region, locate…

2007 Science
Hinode SOHO 208
The Variable Rotation Period of the Inner Region of Saturn’s Plasma Disk
DOI: 10.1126/science.1138562 Bibcode: 2007Sci...316..442G

Gurnett, D. A.; Persoon, A. M.; Dougherty, M. K. +4 more

We show that the plasma and magnetic fields in the inner region of Saturn’s plasma disk rotate in synchronism with the time-variable modulation period of Saturn’s kilometric radio emission. This relation suggests that the radio modulation has its origins in the inner region of the plasma disk, most likely from a centrifugally driven convective ins…

2007 Science
Cassini 205