JP 3-50 National Search and Rescue Manual Vol I - US Navy
JP 3-50 National Search and Rescue Manual Vol I - US Navy JP 3-50 National Search and Rescue Manual Vol I - US Navy
known, or a yacht is on an extended coastal or ocean cruise. The datum area may be readily apparent. In other cases, the area can be narrowed by communications checks and deduction; if not, large general areas may have to be searched. 512 Computation of Datum A. Drift is movement of a search object caused by external forces. Datum is calculated by determining which drift forces will affect the search object, selecting the most appropriate ones, and calculating a vector for each. The vectors are then added to the initial position to determine datum. Drift forces should be calculated using the time between the last known position and a time selected by the SMC. This time of datum is normally chosen to coincide with the daily maximum search effort, using midsearch time or the first SRU arrival time. B. The SMC should determine which environmental forces affected the search object during and after the incident: 1. For marine incidents, currents and winds. 2. For aircraft, primarily wind. 3. For lost persons, terrain and meteorological conditions. C. The SMC should attempt to quantify each force affecting drift, which is best done by vector, with bearing and length of the vector representing target direction and speed respectively. Since objects that float or fly are more affected by environmental forces, it is easier to quantify their possible movement. Lost persons, while affected by the environment, may choose or not choose to move, or may move unpredictably. D. Surface drift forces that act on the target are plotted as shown in Figure 5-3. Since all drift elements are acting simultaneously on the object, the path is along the resultant vector. Lengths of vectors are measured in units of distance. Drift speed information is converted to distance covered in a given time period. To determine force vectors: 1. Determine speed of the environmental force. 2. Convert force speed to object speed. 3. Multiply object speed by duration of drift to determine vector length. 4. Determine force direction. 5. Convert force direction to object direction. 6. Add all object vectors to derive the resultant motion vector of the object.
Figure 5-3. Vector Plots of Surface Drift Forces 513 Aerospace Drift (Da) A. Aircraft Glide, the maximum ground distance that an aircraft could cover during descent, should be determined if the position and altitude of an aircraft engine failure are known and crew bailout is doubtful. Aircraft glide ratio and rate of descent should be obtained from the parent agency or aircraft performance manual. The SMC can then determine maximum ground distance covered during descent and establish the possible area of impact after adjusting for wind (see Figure 5-1). A circle is constructed around the corrected last known position, using maximum no-wind glide distance as the radius. The enclosed area will be the maximum possible area for the aircraft datum. 5-4
- Page 71 and 72: continental U.S. and at offshore lo
- Page 73 and 74: the potential for recording data wi
- Page 75 and 76: other craft or radio stations: 1. A
- Page 77 and 78: EPIRBs. 9. 27.065 kHz (Citizens Ban
- Page 79 and 80: vessels) will be required to carry
- Page 81 and 82: . Non-compliance with FCC Rules and
- Page 83 and 84: 9. SART. 10. MF DSC, used to initia
- Page 85 and 86: 4. FAA Domestic Teletype Networks,
- Page 87 and 88: 3023 kHz (USB), 123.1 MHz, and 282.
- Page 89 and 90: 3. 2638 kHz, all areas. 4. 2738 kHz
- Page 91 and 92: SRUs and agencies. A search action
- Page 93 and 94: 2. Rescue Area f. SRUs on scene a.
- Page 95 and 96: extended time, a Notice to Mariners
- Page 97 and 98: The receiving and recording of info
- Page 99 and 100: case. The SMC is often automaticall
- Page 101 and 102: any source. b. There is suspicion t
- Page 103 and 104: The craft's float or flight plan is
- Page 105 and 106: Figure 4-1. Water Chill Without Ant
- Page 107 and 108: s Figure 4-2. Wind Chill Graph - Eq
- Page 109 and 110: 445 Weather A. Weather may limit SA
- Page 111 and 112: 451 Uncertainty Phase An Emergency
- Page 113 and 114: 471 PRECOM A. PRECOM search contact
- Page 115 and 116: the objective during their normal o
- Page 117 and 118: effective search plan. The plan may
- Page 119 and 120: D. Other SAR planning models, such
- Page 121: 1. The aircraft glide area shown in
- Page 125 and 126: TABLE 5-1. Parachute Drift Distance
- Page 127 and 128: the search object has, the greater
- Page 129 and 130: B. Sea Current (SC) is the residual
- Page 131 and 132: Figure 5-6A. Wind Current - North L
- Page 133 and 134: large lake can vary with season, we
- Page 135 and 136: 5. Other on scene observations can
- Page 137 and 138: 520 SEARCH AREA Figure 5-8. Minimax
- Page 139 and 140: Figure 5-9. Drift Error by Minimax
- Page 141 and 142: DRe to determine SRU error (Y = Fix
- Page 143 and 144: Figure 5-11. Search Areas - Moving
- Page 145 and 146: E. When only a datum area exists, s
- Page 147 and 148: SRUs are dispatched next. Supplemen
- Page 149 and 150: B. POD can be increased by decreasi
- Page 151 and 152: C. Visual sweep widths are determin
- Page 153 and 154: TABLE 5-6. Visual Sweep Width Estim
- Page 155 and 156: 9. Fatigue. Degradation of detectio
- Page 157 and 158: Table 5-8. Height of Eye vs. Horizo
- Page 159 and 160: 6. Sweep widths for Side-Looking Ai
- Page 161 and 162: TABLE 5-11a. Sweep Widths for Forwa
- Page 163 and 164: Sweep widths should be approximated
- Page 165 and 166: TABLE 5-14. Environmental Limitatio
- Page 167 and 168: Figure 5-19. Maritime Probability o
- Page 169 and 170: again, unless it is determined furt
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known, or a yacht is on an extended coastal or ocean cruise.<br />
The datum area may be readily apparent. In other cases, the<br />
area can be narrowed by communications checks <strong>and</strong> deduction;<br />
if not, large general areas may have to be searched.<br />
512 Computation of Datum<br />
A. Drift is movement of a search object caused by external forces.<br />
Datum is calculated by determining which drift forces will affect the<br />
search object, selecting the most appropriate ones, <strong>and</strong> calculating a<br />
vector for each. The vectors are then added to the initial position to<br />
determine datum. Drift forces should be calculated using the time<br />
between the last known position <strong>and</strong> a time selected by the SMC. This<br />
time of datum is normally chosen to coincide with the daily maximum<br />
search effort, using midsearch time or the first SRU arrival time.<br />
B. The SMC should determine which environmental forces affected<br />
the search object during <strong>and</strong> after the incident:<br />
1. For marine incidents, currents <strong>and</strong> winds.<br />
2. For aircraft, primarily wind.<br />
3. For lost persons, terrain <strong>and</strong> meteorological conditions.<br />
C. The SMC should attempt to quantify each force affecting drift,<br />
which is best done by vector, with bearing <strong>and</strong> length of the vector<br />
representing target direction <strong>and</strong> speed respectively. Since objects<br />
that float or fly are more affected by environmental forces, it is<br />
easier to quantify their possible movement. Lost persons, while<br />
affected by the environment, may choose or not choose to move, or may<br />
move unpredictably.<br />
D. Surface drift forces that act on the target are plotted as<br />
shown in Figure 5-3. Since all drift elements are acting simultaneously<br />
on the object, the path is along the resultant vector. Lengths of<br />
vectors are measured in units of distance. Drift speed information is<br />
converted to distance covered in a given time period. To determine<br />
force vectors:<br />
1. Determine speed of the environmental force.<br />
2. Convert force speed to object speed.<br />
3. Multiply object speed by duration of drift to determine vector<br />
length.<br />
4. Determine force direction.<br />
5. Convert force direction to object direction.<br />
6. Add all object vectors to derive the resultant motion vector<br />
of the object.