User manual SUUNTO ADVIZOR

[. . . ] 6 If hiking from a level of 5, 000 ft down hill to 3, 000 ft and then back up to 8, 000 feet, how is the Wristop Computer going to read this or average it out?7 Why does the vertical ascent/descent measurement show different readings even though I am inside and staying in the same room?2 Where do I find the correct declination for my area so I can set my Wristop Computer?The outdoor enthusiast who enjoys venturing out into sports like skiing, kayaking, mountain climbing, hiking and biking can rely on the Advizor/Metrons accuracy. [. . . ] refer to Section 2 Heart Rate Monitor for details in setting and activiting this feature. When wearing the belt, the current time can be viewed for 10 seconds by pressing the [+] button. If the belt is not worn, the current time is shown on the bottom row (Field 3), in place of the heart rate. IMPORTANT NOTE: In order to set the altitude in the Altimeter mode, the altitude must be known. That information can be found by utilizing a topographical map identifying the current location with the associated altitude marked. The user can then proceed and follow the instructions, setting the altimeter, provided in the section below. In setting the Altimeter, there are three processes that can be performed: the Reference Altitude (known altitude at the current location); Altitude Alarm (signals the user when a certain altitude, programmed, is reached); and Logbook Recording Interval (allows the user to view the altitude, average rate of vertical movement and heart rate within a chosen interval of time). At the desired reference altitude, either PRESS the [Mode] button to accept the changes and return to the main mode or PRESS the [Select] button to move to the next setting. PRESS either the [+] or the [-] button to toggle between the ON and OFF for the Altitude Alarm. At the desired setting, PRESS the [Select] button to move to the next setting. At the desired altitude, either PRESS the [Mode] button to accept the changes and return to the main mode or PRESS the [Select] button to move to the next setting. 27): Field 1 displays the vertical ascent or descent rate; Field 2 displays the current altitude in increments of 5 meters or 10 feet, depending on the unit of measure selected ; and Field 3 displays the particular hour and to the left the text memory. The Outer Circumference displays graphically the altitude in hundreds of meters or feet over a full thousand where one complete circle is equivalent to 1000. PRESS the [-] button to scroll back down in increments of one hour and view the vertical ascent/descent rate and the altitude for that particular hour. In the Altimeter mode, PRESS the [Select] button three times to enter this sub mode. The displays automatically rotate showing the first display for 7 seconds then proceeds to show the next displays at 4 second intervals. 28): Field 1 displays the year; Field 2 displays the text LO with the current logbook number flashing; and Field 3 displays the month and day of the particular logbook number. The user can PRESS the [-] to scroll down to view previous logs captured and then PRESS [+] to scroll up to view the most current logbook. The second display shows the ascent information for the particular logbook that is being viewed (Fig. Field 1 displays the average vertical ascent rate during the event; Field 2 displays the total vertical ascent ; and Field 3 displays the text ASC along with the text Log Book to the left. Field 1 displays the average vertical descent rate during the event; Field 2 displays the total vertical descent; and Field 3 displays the text dSC along with the text Log Book to the left. The third display shows the descent information for the particular logbook that is being viewed (Fig. [. . . ] Consequently the air pressure difference between two altitudes is also dependant on temperature. Altitude (ft) above sea level 0 656 1312 1969 2625 3281 3937 4593 5250 5906 6562 7874 9187 9843 11155 12468 13124 14765 16405 18046 19686 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. [. . . ]