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- Q5384723 subject Q6181442.
- Q5384723 subject Q7143444.
- Q5384723 subject Q7478477.
- Q5384723 abstract "In differential geometry, the equivalent latitude is a Lagrangian coordinate .It is often used in atmospheric science,particularly in the study of stratospheric dynamics.Each isoline in a map of equivalent latitude follows the flow velocity and encloses the same area as the latitude line of equivalent value, hence "equivalent latitude." Equivalent latitude is calculated from potential vorticity, from passive tracer simulations and from actual measurements of atmospheric tracers such as ozone.".
- Q5384723 wikiPageWikiLink Q108376.
- Q5384723 wikiPageWikiLink Q1418563.
- Q5384723 wikiPageWikiLink Q188444.
- Q5384723 wikiPageWikiLink Q194404.
- Q5384723 wikiPageWikiLink Q2303697.
- Q5384723 wikiPageWikiLink Q36933.
- Q5384723 wikiPageWikiLink Q5462119.
- Q5384723 wikiPageWikiLink Q6181442.
- Q5384723 wikiPageWikiLink Q6418927.
- Q5384723 wikiPageWikiLink Q7143444.
- Q5384723 wikiPageWikiLink Q7478477.
- Q5384723 wikiPageWikiLink Q757520.
- Q5384723 comment "In differential geometry, the equivalent latitude is a Lagrangian coordinate .It is often used in atmospheric science,particularly in the study of stratospheric dynamics.Each isoline in a map of equivalent latitude follows the flow velocity and encloses the same area as the latitude line of equivalent value, hence "equivalent latitude." Equivalent latitude is calculated from potential vorticity, from passive tracer simulations and from actual measurements of atmospheric tracers such as ozone.".
- Q5384723 label "Equivalent latitude".