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UCL online tools: An application for computing H3+ cooling rate Dugan Witherick / Steve Miller / Nick Achilleos Miracle Computational.

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Presentation on theme: "UCL online tools: An application for computing H3+ cooling rate Dugan Witherick / Steve Miller / Nick Achilleos Miracle Computational."— Presentation transcript:

1 http://europlanet-ri.eu UCL online tools: An application for computing H3+ cooling rate Dugan Witherick / Steve Miller / Nick Achilleos Miracle Computational Officer / Lecturers, Departments of Physics / Science and Technology Studies University College London JRA3 Workshop @ UCL: 22-24 April 2010

2 http://europlanet-ri.eu  What is H3+ ? A molecular ion which strongly radiates in the infrared wavelength region (3-4 micron) - transitions between ro-vibrational levels. Important element of ‘energy budget’ for ionospheres of hydrogen-rich gas giants esp. Jupiter and Saturn. Especially auroral regions. For example:

3 http://europlanet-ri.eu  Aspects of H3+ emission A molecular ion which strongly radiates in the infrared wavelength region (3-4 micron) - transitions between ro-vibrational levels. Important element of ‘energy budget’ for ionospheres of hydrogen-rich gas giants esp. Jupiter and Saturn. Especially auroral regions. For example, Jupiter’s auroral oval radiates of order 10 11 - 10 12 W in the UV and IR bands. Clarke et al, Nature, 2002

4 http://europlanet-ri.eu  Aspects of H3+ emission Departures from LTE become important in determining H3+ emission from the Jovian thermosphere, at altitudes above 500 km (zero-point=1 B level) (Melin et al, Icarus, 2005) Timescales for radiative de-excitation become competitive with collisional de- excitation. By ~2000 km altitude, typical excited vibrn levels have populations <10% of value predicted by LTE ! Example of calculation from Melin et al 2005

5 5JRA3 Workshop @ UCL: 22-24/04/2010 ‘H3PCool’ Introduction to application (source code by S. Miller, deployment over web by D. Witherick) - ‘Home page’:

6 ‘H3PCool’ Introductory text and references, courtesy of Dugan

7 ‘H3PCool’ Input fields for H2 density grid and Temperature grid, email address

8 ‘H3PCool’ Information about requested run received upon ‘click’ for submission

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10 ‘H3PCool’ Email link takes user to several output files. The most basic shows the columns of density, temperature and emission per H3+ molecule in W/str. Can download as ASCII or choose to have the output files sent in an email. Important for accurate interpretation of infrared auroral emissions, in the context of diagnosing auroral/ionospheric conditions. Important input for radiative transfer models and GCMs.


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