Accurately estimating the ocean subsurface salinity structure(OSSS)is crucial for understanding ocean dynamics and predicting climate variations.We present a convolutional neural network(CNN)model to estimate the OSSS...Accurately estimating the ocean subsurface salinity structure(OSSS)is crucial for understanding ocean dynamics and predicting climate variations.We present a convolutional neural network(CNN)model to estimate the OSSS in the Indian Ocean using satellite data and Argo observations.We evaluated the performance of the CNN model in terms of its vertical and spatial distribution,as well as seasonal variation of OSSS estimation.Results demonstrate that the CNN model accurately estimates the most significant salinity features in the Indian Ocean using sea surface data with no significant differences from Argo-derived OSSS.However,the estimation accuracy of the CNN model varies with depth,with the most challenging depth being approximately 70 m,corresponding to the halocline layer.Validations of the CNN model’s accuracy in estimating OSSS in the Indian Ocean are also conducted by comparing Argo observations and CNN model estimations along two selected sections and four selected boxes.The results show that the CNN model effectively captures the seasonal variability of salinity,demonstrating its high performance in salinity estimation using sea surface data.Our analysis reveals that sea surface salinity has the strongest correlation with OSSS in shallow layers,while sea surface height anomaly plays a more significant role in deeper layers.These preliminary results provide valuable insights into the feasibility of estimating OSSS using satellite observations and have implications for studying upper ocean dynamics using machine learning techniques.展开更多
Coastal upwelling is significant for marine ecosystems by lifting nutrient-rich deep waters into the euphotic zone,thereby increasing primary and secondary productivity.The satellite observations show that the norther...Coastal upwelling is significant for marine ecosystems by lifting nutrient-rich deep waters into the euphotic zone,thereby increasing primary and secondary productivity.The satellite observations show that the northern Arafura Sea(NAS),especially in the coastal region,features high chlorophyll-a(chl-a)concentrations,implying a strong coastal upwelling.However,coastal upwelling in the NAS has not received much attention.Based on a semi-automatic image processing technology,the seasonal and interannual variability of coastal upwelling in the NAS are investigated in this study using satellite-observed sea surface temperature(SST)and wind data.The results suggest that there are seasonal coastal upwelling events in the NAS modulated by upwelling-favorable southeast monsoon(SEM).The annual mean days,mean area,and annual mean intensity of coastal upwelling events during the SEM season are 92 days,6514 km^(2),and-5.31×10^(5),respectively,while the corresponding values during the northwest monsoon(NWM)season are 32 days,5569 km^(2),and-1.41×10^(5).It is also found that the SEM coastal upwelling in the NAS displays prominent interannual variability.The strong upwelling events are found in 2010,2013,2016,and 2017 when the southeast monsoon winds were weaker.Further analysis suggests that at the interannual scale,the upwelling index(UI)averaged in the SEM season is negatively correlated with that of three upwelling indicators.This can be attributed to the limitation of onshore geostrophic flow which is evidenced by the negative correlation between the UI and the alongshore difference in sea surface height.This study highlights the important role of the southeast monsoon in the temporal variability of coastal upwelling in the NAS.展开更多
Neptunea cumingii is an important nutrition-rich economic species in China.Juveniles of N.cumingii suff er from high mortality at low temperatures,which has proved a limiting factor in raising seedlings in artifi cial...Neptunea cumingii is an important nutrition-rich economic species in China.Juveniles of N.cumingii suff er from high mortality at low temperatures,which has proved a limiting factor in raising seedlings in artifi cial habitats.Previous research has shown that N.cumingii displays aggregation behavior in response to adverse environmental changes.Therefore,we determined the eff ects of temperature,food,size of juvenile snails,substratum type,and density of juvenile snails on the aggregation behavior of N.cumingii.Results show that,at a low(4°C)or a high(22°C)temperature,juvenile snails adjusted to the inhospitable environment by exhibiting increased aggregation behavior.However,their aggregation behaviors diff ered at these two temperatures.There was no signifi cant diff erence in the aggregation rate,but the typical aggregation size was larger at 4°C than at 22°C.At 10°C or 16°C,aggregation behavior of juvenile snails reduced.Aggregation increased in the satiation treatment at 10°C and 16°C.Small-sized juveniles tended to have higher aggregation rates(92.22%)and a larger typical aggregation size.More juveniles were distributed in the bottom of shaded substrata.A larger typical aggregation size or higher density signifi cantly reduced the mortality of juvenile snails at a low temperature(4°C).These results broaden our understanding of gastropod aggregation behavior and can be used to develop and improve commercial breeding strategies and resource recovery for N.cumingii.展开更多
Upper ocean mixing plays a key role in the atmosphere-ocean heat transfer and sea ice extent and thickness via modulating the upper ocean temperatures in the Arctic Ocean.Observations of diffusivities in the Arctic th...Upper ocean mixing plays a key role in the atmosphere-ocean heat transfer and sea ice extent and thickness via modulating the upper ocean temperatures in the Arctic Ocean.Observations of diffusivities in the Arctic that directly indicate the ocean mixing properties are sparse.Therefore,the spatiotemporal pattern and magnitude of diapycnal diffusivities and kinetic energy dissipation rates in the upper Arctic Ocean are important for atmosphere-ocean heat transfers and sea ice changes.These were first estimated from the Ice-Tethered Profilers dataset(2005–2019)using a strain-based fine-scale parameterization.The resultant mixing properties showed signifi cant geographical inhomogeneity and temporal variability.Diapycnal diff usivities and dissipation rates in the Atlantic sector of the Arctic Ocean were stronger than those on the Pacific side.Mixing in the Atlantic sector increased significantly during the observation period;whereas in the Pacific sector,it weakened before 2011 and then strengthened.Potential impact factors include wind,sea ice,near inertial waves,and stratifi cation,while their relative contributions vary between the two sectors of the Arctic Ocean.In the Atlantic sector,turbulent mixing dominated,while in the Pacific sector,turbulent mixing was inhibited by strong stratification prior to 2011,and is able to overcome the stratifi cation gradually after 2014.The vertical turbulent heat fl ux constantly increased in the Atlantic sector year by year,while it decreased in the Pacific sector post 2010.The estimated heat flux variability induced by enhanced turbulent mixing is expected to continue to diminish sea ice in the near future.展开更多
The generation and propagation characteristics of near-inertial waves(NIWs)generated spontaneously from a quasi-geostrophic anticyclonic mesoscale eddy in a rotating and stratifi ed fl uid were investigated by three-d...The generation and propagation characteristics of near-inertial waves(NIWs)generated spontaneously from a quasi-geostrophic anticyclonic mesoscale eddy in a rotating and stratifi ed fl uid were investigated by three-dimensional numerical modeling.NIWs are generated over a long time interval as a forced response to balanced baroclinic mesoscale eddies.For such eddies,NIW generation from balanced flow is an inevitable result as the evolution of eddies.Moreover,the baroclinicity of mesoscale eddies is an essential condition for this NIW generation mechanism.The spontaneously generated NIWs radiate horizontally toward the eddy center and propagate upward in vertical direction.The forcing of the NIWs moves downward along the eddy axis from the location of maximum temperature anomaly of the mesoscale eddy.The moving speed of the forcing is independent on the balanced mesoscale eddies but is determined by the ratio of buoyancy to inertial frequency.When the forcing reaches the bottom of the mesoscale eddy,the spontaneous NIW generation process terminates.NIW intensity in this spontaneous generation process is strengthened with the increase of the Rossby and Froude numbers.Further research to gain a solid understanding of the role of the Rossby and Froude numbers is necessary for the parameterization of spontaneous NIW generation from quasi-geostrophic mesoscale eddies in general circulation model.展开更多
Metamorphosis is the short developmental stage characterized by dramatic ontogenetic changes that occurs in most animals.However,this important process remains largely unclear in marine invertebrates.In this study,we ...Metamorphosis is the short developmental stage characterized by dramatic ontogenetic changes that occurs in most animals.However,this important process remains largely unclear in marine invertebrates.In this study,we performed the sequential RNA sequencing of a representative mollusk,the rapa whelk(Rapana venosa),that is undergoing metamorphosis and conducted differential gene expression analysis and weighted gene co-expression network analysis(WGCNA)to investigate the overall and dynamic transcriptome responses.The results revealed that the expression of cytochrome P4502A and 3A were upregulated during metamorphosis,while the expression of H/ACA ribonucleoproteins increased 4 h after metamorphosis induction(M4 stage),indicating that R.venosa mainly responded to the pelagobenthic changes.At the M24 stage,the enrichment of V-type proton ATPase and insulin indicated the complete development of secretory organs and initiation of hormone secretion.Furthermore,at the M48 stage,the enrichment of zinc metalloproteinase and conotoxin indicated a well-developed predation system that requires exogenous nutrition.Finally,during the PL stage,the genes associated with growth control were highly enriched,implying that R.venosa had completed metamorphosis and has entered the period of rapid growth.Therefore,our study provides useful transcriptomic resources for R.venosa and contributes new insights that may assist in elucidating the mechanisms underlying metamorphosis in marine invertebrates.展开更多
基金Supported by the National Key Research and Development Program of China(No.2022YFF0801400)the National Natural Science Foundation of China(No.42176010)the Natural Science Foundation of Shandong Province,China(No.ZR2021MD022)。
文摘Accurately estimating the ocean subsurface salinity structure(OSSS)is crucial for understanding ocean dynamics and predicting climate variations.We present a convolutional neural network(CNN)model to estimate the OSSS in the Indian Ocean using satellite data and Argo observations.We evaluated the performance of the CNN model in terms of its vertical and spatial distribution,as well as seasonal variation of OSSS estimation.Results demonstrate that the CNN model accurately estimates the most significant salinity features in the Indian Ocean using sea surface data with no significant differences from Argo-derived OSSS.However,the estimation accuracy of the CNN model varies with depth,with the most challenging depth being approximately 70 m,corresponding to the halocline layer.Validations of the CNN model’s accuracy in estimating OSSS in the Indian Ocean are also conducted by comparing Argo observations and CNN model estimations along two selected sections and four selected boxes.The results show that the CNN model effectively captures the seasonal variability of salinity,demonstrating its high performance in salinity estimation using sea surface data.Our analysis reveals that sea surface salinity has the strongest correlation with OSSS in shallow layers,while sea surface height anomaly plays a more significant role in deeper layers.These preliminary results provide valuable insights into the feasibility of estimating OSSS using satellite observations and have implications for studying upper ocean dynamics using machine learning techniques.
基金Supported by the Strategic Priority Research Program of Chinese Academy of Sciences(No.XDB 42000000)the National Natural Science Foundation of China(No.92258301)+2 种基金the Scientific and Technological Innovation Project financially supported by Laoshan Laboratory(No.LSKJ202202502)the CAS Key Deployment Project of Center for Ocean Mega-Research of Science(No.COMS2020Q07)the CAS-CSIRO Jointly Project(No.133244KYSB20190031)。
文摘Coastal upwelling is significant for marine ecosystems by lifting nutrient-rich deep waters into the euphotic zone,thereby increasing primary and secondary productivity.The satellite observations show that the northern Arafura Sea(NAS),especially in the coastal region,features high chlorophyll-a(chl-a)concentrations,implying a strong coastal upwelling.However,coastal upwelling in the NAS has not received much attention.Based on a semi-automatic image processing technology,the seasonal and interannual variability of coastal upwelling in the NAS are investigated in this study using satellite-observed sea surface temperature(SST)and wind data.The results suggest that there are seasonal coastal upwelling events in the NAS modulated by upwelling-favorable southeast monsoon(SEM).The annual mean days,mean area,and annual mean intensity of coastal upwelling events during the SEM season are 92 days,6514 km^(2),and-5.31×10^(5),respectively,while the corresponding values during the northwest monsoon(NWM)season are 32 days,5569 km^(2),and-1.41×10^(5).It is also found that the SEM coastal upwelling in the NAS displays prominent interannual variability.The strong upwelling events are found in 2010,2013,2016,and 2017 when the southeast monsoon winds were weaker.Further analysis suggests that at the interannual scale,the upwelling index(UI)averaged in the SEM season is negatively correlated with that of three upwelling indicators.This can be attributed to the limitation of onshore geostrophic flow which is evidenced by the negative correlation between the UI and the alongshore difference in sea surface height.This study highlights the important role of the southeast monsoon in the temporal variability of coastal upwelling in the NAS.
基金Supported by the National Key R&D Program of China(No.2019YFD0900800)the fund earmarked for the Modern Agro-industry Technology Research System(No.CARS-49)+5 种基金the Major Scientifi c and Technological Innovation Project of Shandong Provincial Key Research and Development Program(No.2019JZZY020708)the Industry Leading Talents Project of Taishan Scholars(to ZHANG Tao),the Double-Hundred Blue Industry Leader Team of Yantai(to ZHANG Tao)the Construction Technology and Demonstration Application of Dandong Characteristic Beach Type Marine Ranch(No.KFJ-STS-QYZD-189)the Shandong Peninsula Coastal Area Ecological Simulation Test Project:Marine Ranch Resource Evaluation and Sustainable Utilization Model ResearchNSFC-Shandong Joint Fund for Marine Science Research Centers(No.U1406403)the Creative Team Project of the Laboratory for Marine Ecology and Environmental Science,Qingdao National Laboratory for Marine Science and Technology(No.LMEES-CTSP-2018-1)。
文摘Neptunea cumingii is an important nutrition-rich economic species in China.Juveniles of N.cumingii suff er from high mortality at low temperatures,which has proved a limiting factor in raising seedlings in artifi cial habitats.Previous research has shown that N.cumingii displays aggregation behavior in response to adverse environmental changes.Therefore,we determined the eff ects of temperature,food,size of juvenile snails,substratum type,and density of juvenile snails on the aggregation behavior of N.cumingii.Results show that,at a low(4°C)or a high(22°C)temperature,juvenile snails adjusted to the inhospitable environment by exhibiting increased aggregation behavior.However,their aggregation behaviors diff ered at these two temperatures.There was no signifi cant diff erence in the aggregation rate,but the typical aggregation size was larger at 4°C than at 22°C.At 10°C or 16°C,aggregation behavior of juvenile snails reduced.Aggregation increased in the satiation treatment at 10°C and 16°C.Small-sized juveniles tended to have higher aggregation rates(92.22%)and a larger typical aggregation size.More juveniles were distributed in the bottom of shaded substrata.A larger typical aggregation size or higher density signifi cantly reduced the mortality of juvenile snails at a low temperature(4°C).These results broaden our understanding of gastropod aggregation behavior and can be used to develop and improve commercial breeding strategies and resource recovery for N.cumingii.
基金Supported by the National Key Research and Development Program of China(Nos.2019YFE0105700,2017YFA0604102)the Strategic Priority Research Program of Chinese Academy of Sciences(Nos.XDB42000000,XDA22050202)+2 种基金the National Natural Science Foundation of China(Nos.92058202,41676006,42176244)the Key Deployment Project of Centre for Ocean Mega-Research of Science,Chinese Academy of Sciences(No.COMS2020Q07)the CAS-CSIRO Jointly MHW Project(No.133244KYSB20190031)。
文摘Upper ocean mixing plays a key role in the atmosphere-ocean heat transfer and sea ice extent and thickness via modulating the upper ocean temperatures in the Arctic Ocean.Observations of diffusivities in the Arctic that directly indicate the ocean mixing properties are sparse.Therefore,the spatiotemporal pattern and magnitude of diapycnal diffusivities and kinetic energy dissipation rates in the upper Arctic Ocean are important for atmosphere-ocean heat transfers and sea ice changes.These were first estimated from the Ice-Tethered Profilers dataset(2005–2019)using a strain-based fine-scale parameterization.The resultant mixing properties showed signifi cant geographical inhomogeneity and temporal variability.Diapycnal diff usivities and dissipation rates in the Atlantic sector of the Arctic Ocean were stronger than those on the Pacific side.Mixing in the Atlantic sector increased significantly during the observation period;whereas in the Pacific sector,it weakened before 2011 and then strengthened.Potential impact factors include wind,sea ice,near inertial waves,and stratifi cation,while their relative contributions vary between the two sectors of the Arctic Ocean.In the Atlantic sector,turbulent mixing dominated,while in the Pacific sector,turbulent mixing was inhibited by strong stratification prior to 2011,and is able to overcome the stratifi cation gradually after 2014.The vertical turbulent heat fl ux constantly increased in the Atlantic sector year by year,while it decreased in the Pacific sector post 2010.The estimated heat flux variability induced by enhanced turbulent mixing is expected to continue to diminish sea ice in the near future.
基金Supported by the Strategic Priority Research Program of Chinese Academy of Sciences(Nos.XDA22050202,XDB42000000)the National Natural Science Foundation of China(Nos.92058202,91858103)+3 种基金the National Key Research and Development Program of China(Nos.2017YFA0604102,2016YFC1401404)the CAS Key Research Program of Frontier Sciences(No.QYZDB-SSW-DQC024)the Key Deployment Project of Centre for Ocean Mega-Research of Science,Chinese Academy of Sciences(No.COMS2020Q07)jointly supported by the Chinese Academy of Sciences(CAS)and Commonwealth Scientific and Industrial Research Organisation(CSIRO)(No.133244KYSB20190031)。
文摘The generation and propagation characteristics of near-inertial waves(NIWs)generated spontaneously from a quasi-geostrophic anticyclonic mesoscale eddy in a rotating and stratifi ed fl uid were investigated by three-dimensional numerical modeling.NIWs are generated over a long time interval as a forced response to balanced baroclinic mesoscale eddies.For such eddies,NIW generation from balanced flow is an inevitable result as the evolution of eddies.Moreover,the baroclinicity of mesoscale eddies is an essential condition for this NIW generation mechanism.The spontaneously generated NIWs radiate horizontally toward the eddy center and propagate upward in vertical direction.The forcing of the NIWs moves downward along the eddy axis from the location of maximum temperature anomaly of the mesoscale eddy.The moving speed of the forcing is independent on the balanced mesoscale eddies but is determined by the ratio of buoyancy to inertial frequency.When the forcing reaches the bottom of the mesoscale eddy,the spontaneous NIW generation process terminates.NIW intensity in this spontaneous generation process is strengthened with the increase of the Rossby and Froude numbers.Further research to gain a solid understanding of the role of the Rossby and Froude numbers is necessary for the parameterization of spontaneous NIW generation from quasi-geostrophic mesoscale eddies in general circulation model.
基金supported by the National Natural Science Foundation of China(Grant Nos.32002409,31972814,32002374)the Natural Science Foundation of Shandong Province(Grant No.ZR2019BD003)+6 种基金the China Postdoctoral Science Foundation(Grant No.2021M703248)Young Elite Scientists Sponsorship Program by CAST,2021QNRC001earmarked fund for the Modern Agro-industry Technology Research System(CARS-49)the Major Scientific and Technological Innovation Project of Shandong Provincial Key Research and Development Program(2019JZZY020708)the Industry Leading Talents Project of Taishan Scholars(Recipient:Tao Zhang)the“Double Hundred”Blue Industry Leader Team of Yantai(Recipient:Tao Zhang)the Creative Team Project of the Laboratory for Marine Ecology and Environmental Science,Qingdao National Laboratory for Marine Science and Technology(no.LMEESCTSP-2018-1).
文摘Metamorphosis is the short developmental stage characterized by dramatic ontogenetic changes that occurs in most animals.However,this important process remains largely unclear in marine invertebrates.In this study,we performed the sequential RNA sequencing of a representative mollusk,the rapa whelk(Rapana venosa),that is undergoing metamorphosis and conducted differential gene expression analysis and weighted gene co-expression network analysis(WGCNA)to investigate the overall and dynamic transcriptome responses.The results revealed that the expression of cytochrome P4502A and 3A were upregulated during metamorphosis,while the expression of H/ACA ribonucleoproteins increased 4 h after metamorphosis induction(M4 stage),indicating that R.venosa mainly responded to the pelagobenthic changes.At the M24 stage,the enrichment of V-type proton ATPase and insulin indicated the complete development of secretory organs and initiation of hormone secretion.Furthermore,at the M48 stage,the enrichment of zinc metalloproteinase and conotoxin indicated a well-developed predation system that requires exogenous nutrition.Finally,during the PL stage,the genes associated with growth control were highly enriched,implying that R.venosa had completed metamorphosis and has entered the period of rapid growth.Therefore,our study provides useful transcriptomic resources for R.venosa and contributes new insights that may assist in elucidating the mechanisms underlying metamorphosis in marine invertebrates.
