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Observation of internal wave polarity conversion generated by a rising tide
Author(s) -
Li Lan,
Wang Caixia,
Grimshaw Roger
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl063870
Subject(s) - internal wave , stratification (seeds) , polarity (international relations) , geology , bay , geodesy , internal tide , oceanography , chemistry , biochemistry , cell , seed dormancy , botany , germination , dormancy , biology
The observations reported here are based on time series of in situ observation data in Laoshan Bay off the Qingdao coast. A chain of thermistors (T‐chain) at a fixed location recorded a sequence of elevation internal waves followed by depression internal waves passing by over an elapsed time of about 1 h. This observed polarity conversion at a fixed location is caused by the vertical stratification variation mainly induced by the rising tide, which is believed to be the first reported observation of this kind. The process of an elevation internal wave train converting to a depression wave train is simulated using the variable‐coefficient extended Korteweg‐de Vries (veKdV) equation, which also provides a further comparison between theory and the reported observations.