Response of the upper ocean to tropical cyclone in the Northwest Pacific observed by gliders during fall 2018

The evolution of thermohaline structure at the upper ocean during three tropical cyclones(TCs)in the Northwest Pacific was studied in this study based on successive observation by two new-style underwater gliders during fall 2018.These remote-controllable gliders with CTD sensor enabled us to explore high frequency responses of temperature,salinity,mixed and barrier layers in the upper ocean to severe TCs in this area.Results showed that three significant cooling-to-warming and stratification destructing-to-reconstructing processes at the mixed layer occurred during the lives of three TCs.The maximal cooling of SST all reached≥0.5℃although TCs with different intensities had different minimal distances to the observed area.Under potential impacts of solar radiation,tide and inertial motions,the mixed layer depth possessed significant high-frequency fluctuations during TC periods.In addition,barrier layers appeared and vanished quickly during TCs,accompanied with varied temperature inversion processes.

Dynamical features of near-inertial motions in global ocean based on the GDP dataset from 2000 to 2019

Based on the latest oceanic surface drifter dataset from the global drifter program during 2000–2019,this study investigated the global variation of relative frequency shift(RFS),near-inertial energy(NIE)and inverse excess bandwidth(IEB)of near-inertial motions,and analyzed their relations with oceanic mesoscale dynamics,relative vorticity and strain.Compared with previous works,we have some new findings in this study:(1)the RFS was high with negative values in some regions in which we found a significant blue shift of the RFS in the equatorward of 30°N(S)and from 50°N to 60°N in the Pacific,and a red shift in the western boundary currents and their extension regions,the North Atlantic and the Antarctic Circumpolar Current regions;(2)more peak values of the NIE were found in global regions like the South Indian Ocean,the Luzon Strait and some areas of the South Ocean;(3)the global distribution of the IEB were characterized by clear zonal bands and affected by vorticity and wind field;(4)the RFS was elevated as the absolute value of the gradient of vorticity increased,the IEB did not depend on the gradient of vorticity,and the eddy kinetic energy(EKE)weakened with the decrease of the absolute value of RFS;(5)the NIE decreased with increasing absolute value of the relative vorticity and the gradient of vorticity,but it increased with increasing strain and EKE when EKE was larger than 0.0032 m2/s2.