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.

Physical structure and phytoplankton community off the eastern Hainan coast during summer 2015

Based on satellite remote sensing dataset and survey data during upwelling season of 2015,the spatial structures of phytoplankton biomass and community for the first time in the eastern Hainan upwelling(EHU)and its adjacent area,the eastern Leizhou Peninsula upwelling(ELPU)were illustrated.It is found that a significant cold tongue with high salinity and low temperature along the eastern Hainan coast driven by upwelling-favorable summer monsoon.The ELPU was relative weaker than the EHU because of its wide and gentle continental slope.Due to mixing by tides and waves,DO concentration with high value(>6.0 mg/L)were almost homogenous from surface to 30 m depth at the EHU.Beneath that,low DO water(<6.0 mg/L,anoxia)were pumped upward from bottom by the upwelling.The ELPU has worse DO condition compared with the EHU where bottom DO were lower than 3.5 mg/L owing to abundant DO consumption.The phytoplankton biomass reached maximal value about 1.5 mg/m3 at 30 m depth layer rather than surface layer at the EHU indicating the impact limit of upwelling on phytoplankton growth and DO distribution.Nourished by rich nutrient input,the phytoplankton biomass at the ELPU were much higher than the EHU where the maximal value can reach about 4.0 mg/m3.The phytoplankton biomass were reduced to about 0.2–0.3 mg/m3 at the offshore areas of the EHU and ELPU which were close to the value at open sea.At the inshore of the EHU,the phytoplankton community was dominated by diatom which accounted for about 50%of phytoplankton biomass.And prokaryotes(about 40%),green algae(about 20%)and prochlorococcus(about 20%)became main species at the offshore of the EHU.At the ELPU,diatom accounted for about 80%of phytoplankton biomass followed by green algae,indicating a different ecosystem at this region compared with the EHU.