| | 1 | == Observable == |
| | 2 | |
| | 3 | It is in the description of the independent variables, what the data |
| | 4 | in fact measure, that there is the greatest variation in terminology |
| | 5 | among data archives. Most solar observational data consist of direct |
| | 6 | measurements of the intensity of radiation as a function of time, |
| | 7 | direction (location), wavelength, and polarization, or combinations |
| | 8 | of intensities associated with different independent variables (''e.g.'' |
| | 9 | line shifts and splittings, Stokes parameters). These data may be |
| | 10 | interpreted as measurements of certain physical observables, such as |
| | 11 | temperature, velocity, emission measure, etc. via models. There are |
| | 12 | of course some important exceptions: some solar data archives include |
| | 13 | ''in situ'' measurements of such observables as particle fluxes and |
| | 14 | compositions and magnetic field strengths; some solar data sets represent |
| | 15 | not direct observation but the results of complex inversions or modeling, |
| | 16 | such as the frequencies of acoustic modes, or the interior structure; |
| | 17 | and there are catalogs, histories, and descriptions of features and events. |
| | 18 | As long as the various observable classes are orthogonal, however, these |
| | 19 | additional cases should present no problem. |
| | 20 | |
| | 21 | |
| | 22 | The model of describing observables in terms of particular combinations |
| | 23 | of intensity measurements or the associated physical parameters to be derived |
| | 24 | from them is a natural one for data deriving from imaging spectrographs, |
| | 25 | such as magnetographs and helioseismic instruments. For cameras or |
| | 26 | radiometers measuring only intensity or flux at selected wavelengths, |
| | 27 | it is not so natural. People dealing with data from such instruments |
| | 28 | tend to think of the observables as being associated with the spectral |
| | 29 | wavelength or band selected, or for monochromatic instruments, even the |
| | 30 | spatial-temporal target of the observations. It is important to |
| | 31 | understand that the meaning of the term "observable" in the VSO Search |
| | 32 | Parameter model may not at all agree with the meaning of the term as |
| | 33 | used by the data providers. |
| | 34 | |
| | 35 | |
| | 36 | |
| | 37 | |
| | 38 | ==== Physical_Observable ==== |
| | 39 | |
| | 40 | |
| | 41 | type: ''menu''[[BR]] |
| | 42 | FITS keyword: ''PHYS_OBS''[[BR]] |
| | 43 | The following values are currently recognized: |
| | 44 | |
| | 45 | |
| | 46 | ''' intensity ''' |
| | 47 | |
| | 48 | |
| | 49 | the direct intensity, either integrated over the spectral observing range |
| | 50 | or as a function of wavelength (spectral density) |
| | 51 | |
| | 52 | |
| | 53 | ''' equivalent_width ''' |
| | 54 | |
| | 55 | |
| | 56 | differences between intensities measured at nerbay wavelengths, |
| | 57 | typically in line cores, wings, and nearby continuum, whether measured |
| | 58 | as an intensity difference or an equivalent width |
| | 59 | |
| | 60 | ''' polarization_vector ''' |
| | 61 | |
| | 62 | |
| | 63 | the net linear polarization |
| | 64 | |
| | 65 | ''' LOS_magnetic_field ''' |
| | 66 | |
| | 67 | |
| | 68 | the frequency/wavelength Zeeman splitting between opposite circular |
| | 69 | polarizations of a magnetically-sensitive line |
| | 70 | |
| | 71 | ''' vector_magnetic_field ''' |
| | 72 | |
| | 73 | |
| | 74 | field strengths and directions inferred from Stokes polarimetry |
| | 75 | |
| | 76 | ''' LOS_velocity ''' |
| | 77 | |
| | 78 | |
| | 79 | the displacement of line center from rest wavelength/frequency in |
| | 80 | an arbitrary polarization state |
| | 81 | |
| | 82 | ''' vector_velocity ''' |
| | 83 | |
| | 84 | |
| | 85 | two- or three-dimesnional velocities, typically inferred from |
| | 86 | helioseismic inversion or from directly measured velocities transverse |
| | 87 | to the line of sight, possibly combined with Doppler velocities |
| | 88 | |
| | 89 | ''' wave_power ''' |
| | 90 | |
| | 91 | |
| | 92 | |
| | 93 | ''' wave_phase ''' |
| | 94 | |
| | 95 | |
| | 96 | |
| | 97 | ''' oscillation_mode_parameters ''' |
| | 98 | |
| | 99 | |
| | 100 | These all refer to solar internal or atmospheric acoustic-gravity wave |
| | 101 | measurements. The mode parameters could include frequencies, splittings, |
| | 102 | amplitudes, widths, ''etc.'' |
| | 103 | |
| | 104 | ''' number_density ''' |
| | 105 | |
| | 106 | ''' particle_flux ''' |
| | 107 | |
| | 108 | ''' composition ''' |
| | 109 | |
| | 110 | ''' particle_velocity ''' |
| | 111 | |
| | 112 | ''' thermal_velocity ''' |
| | 113 | |
| | 114 | |
| | 115 | ''' ''in-situ'' observations ''' |
| | 116 | |
| | 117 | |
| | 118 | In addition to the above, the following classes have been suggested: |
| | 119 | |
| | 120 | |
| | 121 | * Electric Field Strength - the Stark effect splitting |
| | 122 | * Transverse Magnetic Field Strength - Hanle effect measurements |
| | 123 | * Stokes Parameters ('''I, Q, U, V''' - equivalent to observables of net circular, linear and total polarization, and polarization angle |
| | 124 | * ''in situ'' Magnetic Field |
| | 125 | * Differential Emission Measure |
| | 126 | * Model Parameters - Interior, Atmosphere, Solar Wind |