1 | /*
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2 | *+
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3 | * Name:
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4 | * palPlante
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5 |
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6 | * Purpose:
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7 | * Topocentric RA,Dec of a Solar-System object from heliocentric orbital elements
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8 |
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9 | * Language:
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10 | * Starlink ANSI C
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11 |
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12 | * Type of Module:
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13 | * Library routine
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14 |
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15 | * Invocation:
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16 | * void palPlante ( double date, double elong, double phi, int jform,
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17 | * double epoch, double orbinc, double anode, double perih,
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18 | * double aorq, double e, double aorl, double dm,
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19 | * double *ra, double *dec, double *r, int *jstat );
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20 |
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21 |
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22 | * Description:
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23 | * Topocentric apparent RA,Dec of a Solar-System object whose
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24 | * heliocentric orbital elements are known.
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25 |
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26 | * Arguments:
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27 | * date = double (Given)
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28 | * TT MJD of observation (JD-2400000.5)
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29 | * elong = double (Given)
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30 | * Observer's east longitude (radians)
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31 | * phi = double (Given)
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32 | * Observer's geodetic latitude (radians)
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33 | * jform = int (Given)
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34 | * Element set actually returned (1-3; Note 6)
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35 | * epoch = double (Given)
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36 | * Epoch of elements (TT MJD)
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37 | * orbinc = double (Given)
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38 | * inclination (radians)
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39 | * anode = double (Given)
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40 | * longitude of the ascending node (radians)
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41 | * perih = double (Given)
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42 | * longitude or argument of perihelion (radians)
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43 | * aorq = double (Given)
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44 | * mean distance or perihelion distance (AU)
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45 | * e = double (Given)
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46 | * eccentricity
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47 | * aorl = double (Given)
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48 | * mean anomaly or longitude (radians, JFORM=1,2 only)
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49 | * dm = double (Given)
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50 | * daily motion (radians, JFORM=1 only)
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51 | * ra = double * (Returned)
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52 | * Topocentric apparent RA (radians)
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53 | * dec = double * (Returned)
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54 | * Topocentric apparent Dec (radians)
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55 | * r = double * (Returned)
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56 | * Distance from observer (AU)
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57 | * jstat = int * (Returned)
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58 | * status: 0 = OK
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59 | * - -1 = illegal jform
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60 | * - -2 = illegal e
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61 | * - -3 = illegal aorq
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62 | * - -4 = illegal dm
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63 | * - -5 = numerical error
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64 |
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65 | * Authors:
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66 | * PTW: Pat Wallace (STFC)
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67 | * TIMJ: Tim Jenness (JAC, Hawaii)
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68 | * {enter_new_authors_here}
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69 |
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70 | * Notes:
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71 | * - DATE is the instant for which the prediction is required. It is
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72 | * in the TT timescale (formerly Ephemeris Time, ET) and is a
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73 | * Modified Julian Date (JD-2400000.5).
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74 | * - The longitude and latitude allow correction for geocentric
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75 | * parallax. This is usually a small effect, but can become
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76 | * important for near-Earth asteroids. Geocentric positions can be
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77 | * generated by appropriate use of routines palEpv (or palEvp) and
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78 | * palUe2pv.
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79 | * - The elements are with respect to the J2000 ecliptic and equinox.
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80 | * - A choice of three different element-set options is available:
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81 | *
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82 | * Option JFORM = 1, suitable for the major planets:
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83 | *
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84 | * EPOCH = epoch of elements (TT MJD)
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85 | * ORBINC = inclination i (radians)
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86 | * ANODE = longitude of the ascending node, big omega (radians)
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87 | * PERIH = longitude of perihelion, curly pi (radians)
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88 | * AORQ = mean distance, a (AU)
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89 | * E = eccentricity, e (range 0 to <1)
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90 | * AORL = mean longitude L (radians)
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91 | * DM = daily motion (radians)
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92 | *
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93 | * Option JFORM = 2, suitable for minor planets:
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94 | *
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95 | * EPOCH = epoch of elements (TT MJD)
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96 | * ORBINC = inclination i (radians)
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97 | * ANODE = longitude of the ascending node, big omega (radians)
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98 | * PERIH = argument of perihelion, little omega (radians)
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99 | * AORQ = mean distance, a (AU)
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100 | * E = eccentricity, e (range 0 to <1)
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101 | * AORL = mean anomaly M (radians)
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102 | *
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103 | * Option JFORM = 3, suitable for comets:
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104 | *
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105 | * EPOCH = epoch of elements and perihelion (TT MJD)
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106 | * ORBINC = inclination i (radians)
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107 | * ANODE = longitude of the ascending node, big omega (radians)
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108 | * PERIH = argument of perihelion, little omega (radians)
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109 | * AORQ = perihelion distance, q (AU)
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110 | * E = eccentricity, e (range 0 to 10)
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111 | *
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112 | * Unused arguments (DM for JFORM=2, AORL and DM for JFORM=3) are not
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113 | * accessed.
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114 | * - Each of the three element sets defines an unperturbed heliocentric
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115 | * orbit. For a given epoch of observation, the position of the body
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116 | * in its orbit can be predicted from these elements, which are
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117 | * called "osculating elements", using standard two-body analytical
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118 | * solutions. However, due to planetary perturbations, a given set
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119 | * of osculating elements remains usable for only as long as the
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120 | * unperturbed orbit that it describes is an adequate approximation
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121 | * to reality. Attached to such a set of elements is a date called
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122 | * the "osculating epoch", at which the elements are, momentarily,
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123 | * a perfect representation of the instantaneous position and
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124 | * velocity of the body.
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125 | *
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126 | * Therefore, for any given problem there are up to three different
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127 | * epochs in play, and it is vital to distinguish clearly between
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128 | * them:
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129 | *
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130 | * . The epoch of observation: the moment in time for which the
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131 | * position of the body is to be predicted.
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132 | *
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133 | * . The epoch defining the position of the body: the moment in time
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134 | * at which, in the absence of purturbations, the specified
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135 | * position (mean longitude, mean anomaly, or perihelion) is
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136 | * reached.
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137 | *
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138 | * . The osculating epoch: the moment in time at which the given
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139 | * elements are correct.
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140 | *
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141 | * For the major-planet and minor-planet cases it is usual to make
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142 | * the epoch that defines the position of the body the same as the
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143 | * epoch of osculation. Thus, only two different epochs are
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144 | * involved: the epoch of the elements and the epoch of observation.
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145 | *
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146 | * For comets, the epoch of perihelion fixes the position in the
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147 | * orbit and in general a different epoch of osculation will be
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148 | * chosen. Thus, all three types of epoch are involved.
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149 | *
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150 | * For the present routine:
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151 | *
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152 | * . The epoch of observation is the argument DATE.
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153 | *
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154 | * . The epoch defining the position of the body is the argument
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155 | * EPOCH.
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156 | *
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157 | * . The osculating epoch is not used and is assumed to be close
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158 | * enough to the epoch of observation to deliver adequate accuracy.
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159 | * If not, a preliminary call to palPertel may be used to update
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160 | * the element-set (and its associated osculating epoch) by
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161 | * applying planetary perturbations.
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162 | * - Two important sources for orbital elements are Horizons, operated
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163 | * by the Jet Propulsion Laboratory, Pasadena, and the Minor Planet
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164 | * Center, operated by the Center for Astrophysics, Harvard.
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165 | *
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166 | * The JPL Horizons elements (heliocentric, J2000 ecliptic and
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167 | * equinox) correspond to PAL/SLALIB arguments as follows.
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168 | *
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169 | * Major planets:
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170 | *
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171 | * JFORM = 1
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172 | * EPOCH = JDCT-2400000.5
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173 | * ORBINC = IN (in radians)
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174 | * ANODE = OM (in radians)
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175 | * PERIH = OM+W (in radians)
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176 | * AORQ = A
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177 | * E = EC
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178 | * AORL = MA+OM+W (in radians)
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179 | * DM = N (in radians)
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180 | *
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181 | * Epoch of osculation = JDCT-2400000.5
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182 | *
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183 | * Minor planets:
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184 | *
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185 | * JFORM = 2
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186 | * EPOCH = JDCT-2400000.5
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187 | * ORBINC = IN (in radians)
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188 | * ANODE = OM (in radians)
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189 | * PERIH = W (in radians)
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190 | * AORQ = A
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191 | * E = EC
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192 | * AORL = MA (in radians)
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193 | *
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194 | * Epoch of osculation = JDCT-2400000.5
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195 | *
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196 | * Comets:
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197 | *
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198 | * JFORM = 3
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199 | * EPOCH = Tp-2400000.5
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200 | * ORBINC = IN (in radians)
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201 | * ANODE = OM (in radians)
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202 | * PERIH = W (in radians)
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203 | * AORQ = QR
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204 | * E = EC
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205 | *
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206 | * Epoch of osculation = JDCT-2400000.5
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207 | *
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208 | * The MPC elements correspond to SLALIB arguments as follows.
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209 | *
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210 | * Minor planets:
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211 | *
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212 | * JFORM = 2
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213 | * EPOCH = Epoch-2400000.5
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214 | * ORBINC = Incl. (in radians)
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215 | * ANODE = Node (in radians)
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216 | * PERIH = Perih. (in radians)
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217 | * AORQ = a
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218 | * E = e
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219 | * AORL = M (in radians)
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220 | *
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221 | * Epoch of osculation = Epoch-2400000.5
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222 | *
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223 | * Comets:
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224 | *
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225 | * JFORM = 3
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226 | * EPOCH = T-2400000.5
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227 | * ORBINC = Incl. (in radians)
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228 | * ANODE = Node. (in radians)
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229 | * PERIH = Perih. (in radians)
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230 | * AORQ = q
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231 | * E = e
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232 | *
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233 | * Epoch of osculation = Epoch-2400000.5
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234 |
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235 | * History:
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236 | * 2012-03-12 (TIMJ):
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237 | * Initial version direct conversion of SLA/F.
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238 | * Adapted with permission from the Fortran SLALIB library.
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239 | * {enter_further_changes_here}
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240 |
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241 | * Copyright:
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242 | * Copyright (C) 2004 Patrick T. Wallace
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243 | * Copyright (C) 2012 Science and Technology Facilities Council.
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244 | * All Rights Reserved.
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245 |
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246 | * Licence:
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247 | * This program is free software; you can redistribute it and/or
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248 | * modify it under the terms of the GNU General Public License as
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249 | * published by the Free Software Foundation; either version 3 of
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250 | * the License, or (at your option) any later version.
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251 | *
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252 | * This program is distributed in the hope that it will be
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253 | * useful, but WITHOUT ANY WARRANTY; without even the implied
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254 | * warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR
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255 | * PURPOSE. See the GNU General Public License for more details.
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256 | *
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257 | * You should have received a copy of the GNU General Public License
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258 | * along with this program; if not, write to the Free Software
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259 | * Foundation, Inc., 51 Franklin Street, Fifth Floor, Boston,
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260 | * MA 02110-1301, USA.
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261 |
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262 | * Bugs:
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263 | * {note_any_bugs_here}
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264 | *-
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265 | */
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266 |
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267 | #include "pal.h"
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268 |
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269 | void palPlante ( double date, double elong, double phi, int jform,
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270 | double epoch, double orbinc, double anode, double perih,
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271 | double aorq, double e, double aorl, double dm,
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272 | double *ra, double *dec, double *r, int *jstat ) {
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273 |
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274 | double u[13];
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275 |
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276 | /* Transform conventional elements to universal elements */
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277 | palEl2ue( date, jform, epoch, orbinc, anode, perih, aorq, e, aorl,
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278 | dm, u, jstat );
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279 |
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280 | /* If succcessful, make the prediction */
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281 | if (*jstat == 0) palPlantu( date, elong, phi, u, ra, dec, r, jstat );
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282 |
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283 | }
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284 |
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285 |
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286 |
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