Acta Physica Sinica, Volume. 69, Issue 9, 090201-1(2020)
Fig. 1. Temporal distribution of the number of occultation profiles in January, April, July and October, 2007−2011.
Fig. 3. Angle gradient profile obtained by the difference method and the model function method using the bending angle gradient profile (, boundary layer top height
; (b) bending angle profile with uniform random error
, boundary layer top height
; (c) bending angle profile with uniform random error
, boundary layer top height
; (d) bending angle profile with uniform random error
, boundary layer top height
.
Fig. 4. Height of the boundary layer obtained by the three methods: (a) Three methods to get the height of the boundary layer top based on profile 1,
Fig. 5. The 5-year average boundary layer height of the ocean obtained by the model function method, the data used is the bending angle profile of the four months of 2007−2011 in January, April, July, and October: (a) The average height of the boundary layer in January; (b) the average height of the boundary layer in April; (c) the average height of the boundary layer in July; (d) the average height of the boundary layer in October.
Fig. 6. The 5-year average boundary layer height of the ocean obtained by the model function method, the data used is the zbalmax provided by CDAAC of the four months of 2007−2011 in January, April, July, and October: (a) The average height of the boundary layer in January; (b) the average height of the boundary layer in April; (c) the average height of the boundary layer in July; (d) the average height of the boundary layer in October.
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Jian-Yin Zhou, Jie Xiang, Si-Xun Huang.
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Received: Dec. 29, 2019
Accepted: --
Published Online: Nov. 26, 2020
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