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Magnetic declination is the angle between true north or astronomic north and magnetic north. This angle arises because Earth's magnetic poles do not align with its geographic poles.
The magnetic declination varies by location and changes over time due to shifts in Earth's magnetic field.
Declination may be either east or west. Eastern declination occurs when the magnetic north lies east of the true north, while western declination occurs when it lies to the west.
This variation can affect compass readings, making it crucial for surveyors to account for the declination when determining directions.
The changes in magnetic declination can occur over long periods, known as secular variation, lasting roughly 150 years per cycle.
Additional variations include annual and daily changes, though these are smaller and often negligible for most applications.
Magnetic declination calculators use location and date as inputs to determine accurate declination values for specific areas, which is essential for updating old survey data or conducting precise land surveys.
磁偏角是与地球自转轴对齐的真北方向与跟随地球磁场方向的磁北方向之间的夹角。这种差异的存在是因为磁极与地理极点不一致。磁偏角的值取决于观察者在地球上的位置,并且由于地球磁场的动态特性而随时间变化。
当磁北方向位于真北方向以东时,磁偏角称为东偏角。相反,当磁北方向位于真北方向以西时,磁偏角称为西偏角。理…