Instruction Manual

1800 5906 3.3 37.9

2000 6562 2.0 35.6

2400 7874 -0.6 30.9

2800 9187 -3.2 26.2

3000 9843 -4.5 23.9

3400 11155 -7.1 19.2

3800 12468 -9.7 14.5

4000 13124 -11.0 12.2

4500 14765 -14.3 6.4

5000 16405 -17.5 0.5

5500 18046 -20.8 -5.4

6000 19686 -24.0 -11.2

Table 1. Normal temperatures corresponding to different altitudes

Now the altitude measurement error caused by an abnormal temperature gradient can be approximated as

follows. If the sum of the temperature offsets from the normal temperatures determined at two different

altitudes is 1 ºC, the altitude difference calculated by Wristop Computer is 0.2% off the real altitude

difference (When using imperial units the offset factor is 0.11% / 1 ºF). This is because the real temperatures

are not always the same as the normal temperatures. A higher than normal temperature causes the calculated

altitude difference to be smaller than the real altitude difference (your mountain ascent was actually higher).

Consequently, a lower than normal temperature causes the calculated altitude difference to be larger than the

real altitude difference (you did not ascend quite as high as displayed).

Table 2 shows an example in which the temperature offsets are positive. In this example, the reference altitude

is set at 1000 m. At 3000 m the altitude difference is 2000 m and Wristop Computer shows 80 m too little (20

ºC * 2000 m * 0.002/ºC = 80 m). Your actual altitude is thus 3080 m.