Introduction to Ocean Climate

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Ocean Climate sentence examples within Indian Ocean Climate

Indian Ocean Climate

The multidecadal variability of Indian Ocean sea surface temperature (IOSST) has an important impact on both the regional Indian Ocean climate and the global climate.

Origin of Indian Ocean multidecadal climate variability: role of the North Atlantic Oscillation

Indian Ocean Climate

Hence, this study implies millennial-scale hydroclimate change linked with atmospheric CO2 forcing that could improve our knowledge of the role of atmospheric CO2 in triggering abrupt Indian Ocean climate changes.

Warming trend during millennial-scale cold events in the northern Indian Ocean and potential atmospheric CO2 forcing during the past 40 kyr

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Ocean Climate sentence examples within Southern Ocean Climate

Southern Ocean Climate

Antarctic glacial meltwater likely plays an important role in determining large-scale Southern Ocean climate trends, yet recent modeling efforts have proceeded without a good understanding of how its vertical distribution in the water column is set.

On the settling depth of meltwater escaping from beneath Antarctic ice shelves

Southern Ocean Climate

Together, these analyses highlight dramatic, ecosystem-wide responses to past Southern Ocean climate change and suggest potential for further shifts as warming continues.

Receding ice drove parallel expansions in Southern Ocean penguins

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Ocean Climate sentence examples within Improved Ocean Climate

Improved Ocean Climate

With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea level, mostly due to increased model resolution and updates in assimilated observation data sets.

The ECMWF operational ensemble reanalysis–analysis system for ocean and sea ice: a description of the system and assessment

Improved Ocean Climate

With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea-level, mostly due to increased model resolution and updates in assimilated observation data sets.

The ECMWF operational ensemble reanalysis-analysis system for ocean and sea-ice: a description of the system and assessment

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Ocean Climate sentence examples within Arctic Ocean Climate

Arctic Ocean Climate

ARC3O is therefore capable to realistically translate the simulated Arctic Ocean climate state into one observable quantity for a more comprehensive climate model evaluation and initialization.

The Arctic Ocean Observation Operator for 6.9 GHz (ARC3O) - Part 2: Development and evaluation. In open review for The Cryosphere

Arctic Ocean Climate

An observation operator translates the Arctic Ocean climate simulated by a climate model into a brightness temperature.

Rethinking the relationship between the observed, simulated and real Arctic sea-ice evolution

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Ocean Climate sentence examples within Future Ocean Climate

Future Ocean Climate

Yellowfin bream appear to be highly resilient to predicted near-future ocean climate change, which might be facilitated by their wide spatio-temporal distribution across habitats and broad diet.

Climate change does not affect the seafood quality of a commonly targeted fish

Future Ocean Climate

This adaptive strategy seems to rely on the inherent behavioural response of fishes to their environment and such adjustability shows the kind of responses that organisms may express to prevail in future ocean climate.

Adaptive responses of fishes to climate change: Feedback between physiology and behaviour.

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Ocean Climate sentence examples within Pacific Ocean Climate

Pacific Ocean Climate

The Time‐varying Emulator for Short‐ and Long‐Term analysis of coastal flood hazard potential is presented here as a methodology capable of producing new iterations of the sea‐state parameters associated with the present‐day Pacific Ocean climate to simulate many synthetic extreme compound events.

Time-Varying Emulator for Short and Long-Term Analysis of Coastal Flood Hazard Potential

Pacific Ocean Climate

These indices were compared to the Pacific Decadal Oscillation (PDO), an index of Pacific Ocean climate variability.

The importance of environment and life stage on interpretation of silky shark relative abundance indices for the equatorial Pacific Ocean

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Ocean Climate sentence examples within Tropical Ocean Climate

Tropical Ocean Climate

Leg-1 data from the Japan Agency for Marine-Earth Science and Technology in collaboration with the Agency for the Assessment and Application of Technology which is part of the Tropical Ocean Climate Study Expedition including CTD Yoyo and ADCP taken using ship vehicles R/V Kaiyo.

Analysis of Characteristics and Turbulent Mixing of Seawater Mass in Lombok Strait

Tropical Ocean Climate

Through calculation, we can get storage life of composite in tropical ocean climate and dry heat desert climate environment is from 14.

Storage Life Research on Glass Fiber Reinforced Composite

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Ocean Climate sentence examples within Changing Ocean Climate

Changing Ocean Climate

Identifying refuge areas used by highly mobile species experiencing varying ocean conditions is critical for adaptive marine spatial planning that can accommodate a changing ocean climate.

Spatial and temporal diving behavior of non-breeding common murres during two summers of contrasting ocean conditions

Changing Ocean Climate

Provisioning of meat through aquaculture can be improved via hatchery and breeding advances, a necessity in the changing ocean climate.

Introduction to Provisioning Services

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Ocean Climate sentence examples within ocean climate model

ocean climate model

In this study, the Adriatic Sea and Coast (AdriSC) kilometre-scale atmosphere–ocean climate model covering the Adriatic Sea and northern Ionian Sea is presented.

Performance of the Adriatic Sea and Coast (AdriSC) climate component – a COAWST V3.3-based one-way coupled atmosphere–ocean modelling suite: ocean results

ocean climate model

With the help of dynamical downscaling using a regional coupled atmosphere-ocean climate model, four global Earth System Models were regionalized.

Oceanographic regional climate projections for the Baltic Sea until 2100

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Ocean Climate sentence examples within ocean climate change

ocean climate change

Hence, this study implies millennial-scale hydroclimate change linked with atmospheric CO2 forcing that could improve our knowledge of the role of atmospheric CO2 in triggering abrupt Indian Ocean climate changes.

Warming trend during millennial-scale cold events in the northern Indian Ocean and potential atmospheric CO2 forcing during the past 40 kyr

ocean climate change

Finally, where possible, further research should be combined and contextualized with field-based experiments and observations to better reflect the complexity of marine ecosystems and yield more representative responses to ocean climate change.

Another Decade of Marine Climate Change Experiments: Trends, Progress and Knowledge Gaps

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Ocean Climate sentence examples within ocean climate variability

ocean climate variability

Knowledge about water-mass properties is critical to understanding how ocean climate variability impacts the shelf seas.

A satellite-based Lagrangian view on the origin of water-masses in the northern European shelf seas

ocean climate variability

Elucidating connections between ocean climate variability and change and recruitment of juvenile fishes to adult populations is critical for understanding variability in stock–recruit dynamics.

Source water variability as a driver of rockfish recruitment in the California Current Ecosystem: implications for climate change and fisheries management

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Ocean Climate sentence examples within ocean climate state

ocean climate state

With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea level, mostly due to increased model resolution and updates in assimilated observation data sets.

The ECMWF operational ensemble reanalysis–analysis system for ocean and sea ice: a description of the system and assessment

ocean climate state

ARC3O is therefore capable to realistically translate the simulated Arctic Ocean climate state into one observable quantity for a more comprehensive climate model evaluation and initialization.

The Arctic Ocean Observation Operator for 6.9 GHz (ARC3O) - Part 2: Development and evaluation. In open review for The Cryosphere

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Ocean Climate sentence examples within ocean climate modeling

ocean climate modeling

The ocean surface net radiation (<inline-formula> <tex-math notation="LaTeX">$R_{n}$ </tex-math></inline-formula>) characterizing ocean surface radiation budget is a key variable in ocean climate modeling and analysis.

Generating a High-Resolution Time-Series Ocean Surface Net Radiation Product by Downscaling J-OFURO3

ocean climate modeling

The ocean surface net radiation (Rn) characterizing the ocean surface radiation budget, is a key variable of interest in ocean climate modeling and analysis, which determines the climate model of ocean surface with heat, freshwater and momentum flux.

Downscaling Ocean Surface Net Radiation at Global Scales with Random Forest

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Ocean Climate sentence examples within ocean climate system

ocean climate system

The Amery Ice Shelf (AIS) dynamics and mass balance caused by iceberg calving and basal melting are significant in the ocean climate system.

Analysis of Temporal and Spatial Variability of Fronts on the Amery Ice Shelf Automatically Detected Using Sentinel-1 SAR Data

ocean climate system

This period is too short to evaluate many fundamental aspects of the Antarctic and Southern Ocean climate system, such as decadal-to-century time-scale climate variability and trends.

Back to the future: Using long-term observational and paleo-proxy reconstructions to improve model projections of antarctic climate

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More Ocean Climate sentence examples
10.1088/1742-6596/1731/1/012072

The lack of community understanding of the predictions of the ocean climate is key to addressing the impacts and crisis of the ocean climate.

Development of ARIMA technique in determining the ocean climate prediction skills for pre-service teacher

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10.1371/journal.pone.0244960

Whereas previous studies have shown within-region variability in zooplankton communities in response to ocean climate, we highlight both consistency and change in regional communities, with interannual variability in shelf communities and persistence in community structure offshore.

Spatio-temporal persistence of zooplankton communities in the Gulf of Alaska

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10.2139/ssrn.3912725

On monthly to multi-decadal timescales, there is much uncertainty around the extent to which the non-stationary, non-linear responses of the ice sheets interact through the atmosphere-ocean climate.

Modeling the Interconnectivity of Non-stationary Polar Ice Sheets

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10.1017/S0954102021000067

Our sampled colonies were not panmictic and suggest a lower migration rate, which may reflect relatively stable environmental conditions in the Ross Sea compared to other regions of Antarctica, where the ocean climate is warming.

Genetic diversity in clustered colonies of an Antarctic marine mesopredator: a role for habitat quality?

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10.5194/egusphere-egu21-13159

The fate of surface freshwater is an important factor that modifies ocean stratification, deep water convection and thus, ocean climate.

Wind driven Ekman transport vs eddies – ultimate fight or peaceful cooperation in the Labrador Sea?

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10.1016/J.MARSTRUC.2021.102939

Preservation of fatigue damage during lumping requires an accurate consideration of the met-ocean climate and the dynamic response of the structure.

Environmental lumping for efficient fatigue assessment of large-diameter monopile wind turbines

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10.5194/EGUSPHERE-EGU21-2313

We find that introducing the parameterization of frontal ablation, but ignoring changes in ocean climate, reduces the spread between different emission scenarios in 2100.

Exploring the influence of frontal ablation on global glacier mass change projections

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10.1111/FAF.12356

The method starts from four perspectives: “fisheries management,” “ecosystem,” “ocean climate,” and “global context and governance” for which current status and recent trends are summarized.

A participatory scenario method to explore the future of marine social-ecological systems

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10.5343/bms.2017.1155

The existence of geographical patterns in the composition of platform invertebrate assemblages and the colonization of one platform by a native bryozoan with southern affinities during elevated SST of 2014–2015 suggest that these assemblages may be useful over broad spatial scales as barometers of short- and longer-term changes in ocean climate.

Regional patterns in shallow water invertebrate assemblages on offshore oil and gas platforms along the Pacific continental shelf

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10.1121/1.5136884

The majority of trends derived from Acoustic Thermometry of Ocean Climate (ATOC) systems over nearly two decades, starting at roughly 1994, suggest a decrease in ambient noise levels of up to 1 dB/year.

Comparison of decadal low-frequency ambient noise trends measured in the northern Pacific Ocean: ATOC and CTBTO systems

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10.29006/1564-2291.JOR-2019.47(2).1

In this regard, he was a real encyclopaedist, one of the few in his scientific community, an outstanding expert scientist, who at the highest professional level was engaged in solving the problems of the General circulation of the World ocean, the Interaction of the ocean and atmosphere, Ocean climate, Physics of boundary layers and Wave processes in these two environments, General and particular problems of formation and evolution of the Hydrophysical regime of the ocean.

НАУЧНАЯ СТЕЗЯ Ю.А. ИВАНОВА – ВЫДАЮЩЕГОСЯ РОССИЙСКОГО ЭКСПЕРТА-ЭНЦИКЛОПЕДИСТА В ОБЛАСТИ ГИДРОФИЗИКИ ОКЕАНА

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10.3389/fmars.2019.00103

An annual Report on Ocean Climate (IROC), produced by the WGOH since the late 1990’s, summarizes trends in regional hydrography and identifies patterns linking these changes across the North Atlantic.

The ICES Working Group on Oceanic Hydrography: A Bridge From In-situ Sampling to the Remote Autonomous Observation Era

Keywords related to Ocean

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Ocean Climate
Encyclopedia

What is/are Ocean Climate?

Ocean Climate - The lack of community understanding of the predictions of the ocean climate is key to addressing the impacts and crisis of the ocean climate. [1] Whereas previous studies have shown within-region variability in zooplankton communities in response to ocean climate, we highlight both consistency and change in regional communities, with interannual variability in shelf communities and persistence in community structure offshore. [2] On monthly to multi-decadal timescales, there is much uncertainty around the extent to which the non-stationary, non-linear responses of the ice sheets interact through the atmosphere-ocean climate. [3] Our sampled colonies were not panmictic and suggest a lower migration rate, which may reflect relatively stable environmental conditions in the Ross Sea compared to other regions of Antarctica, where the ocean climate is warming. [4] The fate of surface freshwater is an important factor that modifies ocean stratification, deep water convection and thus, ocean climate. [5] Preservation of fatigue damage during lumping requires an accurate consideration of the met-ocean climate and the dynamic response of the structure. [6] We find that introducing the parameterization of frontal ablation, but ignoring changes in ocean climate, reduces the spread between different emission scenarios in 2100. [7] The method starts from four perspectives: “fisheries management,” “ecosystem,” “ocean climate,” and “global context and governance” for which current status and recent trends are summarized. [8] The existence of geographical patterns in the composition of platform invertebrate assemblages and the colonization of one platform by a native bryozoan with southern affinities during elevated SST of 2014–2015 suggest that these assemblages may be useful over broad spatial scales as barometers of short- and longer-term changes in ocean climate. [9] The majority of trends derived from Acoustic Thermometry of Ocean Climate (ATOC) systems over nearly two decades, starting at roughly 1994, suggest a decrease in ambient noise levels of up to 1 dB/year. [10] In this regard, he was a real encyclopaedist, one of the few in his scientific community, an outstanding expert scientist, who at the highest professional level was engaged in solving the problems of the General circulation of the World ocean, the Interaction of the ocean and atmosphere, Ocean climate, Physics of boundary layers and Wave processes in these two environments, General and particular problems of formation and evolution of the Hydrophysical regime of the ocean. [11] An annual Report on Ocean Climate (IROC), produced by the WGOH since the late 1990’s, summarizes trends in regional hydrography and identifies patterns linking these changes across the North Atlantic. [12]

Indian Ocean Climate

The multidecadal variability of Indian Ocean sea surface temperature (IOSST) has an important impact on both the regional Indian Ocean climate and the global climate. [1] Hence, this study implies millennial-scale hydroclimate change linked with atmospheric CO2 forcing that could improve our knowledge of the role of atmospheric CO2 in triggering abrupt Indian Ocean climate changes. [2] Knowledge of the status of the Indian Ocean climate and ecosystems and predictability of its future, depends on a wide range of socio-economic and environmental data, a significant part of which is provided by IndOOS. [3]

Southern Ocean Climate

Antarctic glacial meltwater likely plays an important role in determining large-scale Southern Ocean climate trends, yet recent modeling efforts have proceeded without a good understanding of how its vertical distribution in the water column is set. [1] Together, these analyses highlight dramatic, ecosystem-wide responses to past Southern Ocean climate change and suggest potential for further shifts as warming continues. [2] This period is too short to evaluate many fundamental aspects of the Antarctic and Southern Ocean climate system, such as decadal-to-century time-scale climate variability and trends. [3]

Improved Ocean Climate

With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea level, mostly due to increased model resolution and updates in assimilated observation data sets. [1] With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea-level, mostly due to increased model resolution and updates in assimilated observation data sets. [2]

Arctic Ocean Climate

ARC3O is therefore capable to realistically translate the simulated Arctic Ocean climate state into one observable quantity for a more comprehensive climate model evaluation and initialization. [1] An observation operator translates the Arctic Ocean climate simulated by a climate model into a brightness temperature. [2]

Future Ocean Climate

Yellowfin bream appear to be highly resilient to predicted near-future ocean climate change, which might be facilitated by their wide spatio-temporal distribution across habitats and broad diet. [1] This adaptive strategy seems to rely on the inherent behavioural response of fishes to their environment and such adjustability shows the kind of responses that organisms may express to prevail in future ocean climate. [2]

Pacific Ocean Climate

The Time‐varying Emulator for Short‐ and Long‐Term analysis of coastal flood hazard potential is presented here as a methodology capable of producing new iterations of the sea‐state parameters associated with the present‐day Pacific Ocean climate to simulate many synthetic extreme compound events. [1] These indices were compared to the Pacific Decadal Oscillation (PDO), an index of Pacific Ocean climate variability. [2]

Tropical Ocean Climate

Leg-1 data from the Japan Agency for Marine-Earth Science and Technology in collaboration with the Agency for the Assessment and Application of Technology which is part of the Tropical Ocean Climate Study Expedition including CTD Yoyo and ADCP taken using ship vehicles R/V Kaiyo. [1] Through calculation, we can get storage life of composite in tropical ocean climate and dry heat desert climate environment is from 14. [2]

Changing Ocean Climate

Identifying refuge areas used by highly mobile species experiencing varying ocean conditions is critical for adaptive marine spatial planning that can accommodate a changing ocean climate. [1] Provisioning of meat through aquaculture can be improved via hatchery and breeding advances, a necessity in the changing ocean climate. [2]

ocean climate model

In this study, the Adriatic Sea and Coast (AdriSC) kilometre-scale atmosphere–ocean climate model covering the Adriatic Sea and northern Ionian Sea is presented. [1] With the help of dynamical downscaling using a regional coupled atmosphere-ocean climate model, four global Earth System Models were regionalized. [2] In this study, the Adriatic Sea and Coast (AdriSC) kilometre-scale atmosphere-ocean climate model covering the Adriatic and northern Ionian Seas is presented. [3] We end with a discussion of the challenges that remain to developing a realistic dynamically adaptive atmosphere or ocean climate models. [4] Forecasting of climate change impacts on marine aquaculture production has become a major research task, which requires taking into account the biases and uncertainties arising from ocean climate models in coastal areas, as well as considering culture management strategies. [5] We end with a discussion of the challenges that remain to developing a realistic dynamically adaptive atmosphere or ocean climate models. [6] We use a coupled atmosphere-ocean climate model to investigate possible effects of different atmospheric CO2 levels and gateway configurations between the North proto-Atlantic Basin and the Arctic Ocean on the formation of Arctic sea-ice in the latest Cretaceous. [7] Most ocean climate models do not represent ice shelf calving in a physically realistic way, even though the calving of icebergs is a major component of the mass balance for Antarctic ice shelves. [8] At the same time, the approach is simple and general enough to be readily implemented in ocean climate models, without adding significant computational cost. [9] Recently available downscaled ocean climate models for the Bering Sea and Aleutian Arc offer the opportunity to assess climate vulnerability for upper trophic level consumers such as marine birds. [10] We conclude that the incorporation of mixing induced by nonbreaking surface waves into FESOM is practically very helpful and suggest that it needs to be considered in other ocean climate models as well. [11] This study investigates the sensitivity of oceanic and atmospheric response in the extra-tropics, especially in the North Pacific, to the position of equatorial El Niño-like heating within a slab-ocean climate model. [12] Here, we investigate the factors controlling R in two atmosphere–slab ocean climate models subjected to a wide range of abrupt climate forcings. [13] Across a range of simulations with a coupled atmosphere–ocean climate model, shifts in the intertropical convergence zone (ITCZ) are induced by an interhemispheric heating contrast. [14] The vertically varying eddy diffusivity can be used to improve parameterization of eddy stirring in the tropical Pacific by coarse-resolution ocean climate models. [15] In all parts of Africa, and especially Eastern Africa where seasonal precipitation variability is a frequent cause huge human suffering due to droughts and famine, the multimodel superensemble and its subsequent improvements will always provide a forecast that outweighs the best Atmosphere-Ocean Climate Model. [16] To represent mixing induced by this turbulence in ocean climate models, the cascade of internal tide energy to dissipation scales must be understood and mapped. [17]

ocean climate change

Hence, this study implies millennial-scale hydroclimate change linked with atmospheric CO2 forcing that could improve our knowledge of the role of atmospheric CO2 in triggering abrupt Indian Ocean climate changes. [1] Finally, where possible, further research should be combined and contextualized with field-based experiments and observations to better reflect the complexity of marine ecosystems and yield more representative responses to ocean climate change. [2] Photophysiological responses of phytoplankton to changing multiple environmental drivers are essential in understanding and predicting ecological consequences of ocean climate changes. [3] Global ocean physical and chemical trends are reviewed and updated using seven key ocean climate change indicators: (i) Sea Surface Temperature, (ii) Ocean Heat Content, (iii) Ocean pH, (iv) Dissolved Oxygen concentration (v) Arctic Sea Ice extent, thickness, and volume (vi) Sea Level and (vii) the strength of the Atlantic Meridional Overturning Circulation (AMOC). [4] The purpose of FAFMIP is to understand and reduce the uncertainty of ocean climate changes in response to increased CO 2 forcing in atmosphere-ocean general circulation models (AOGCMs), including the simulations of ocean heat content (OHC) change, ocean circulation change, and sea level rise due to thermal expansion. [5] Yellowfin bream appear to be highly resilient to predicted near-future ocean climate change, which might be facilitated by their wide spatio-temporal distribution across habitats and broad diet. [6] Together, these analyses highlight dramatic, ecosystem-wide responses to past Southern Ocean climate change and suggest potential for further shifts as warming continues. [7]

ocean climate variability

Knowledge about water-mass properties is critical to understanding how ocean climate variability impacts the shelf seas. [1] Elucidating connections between ocean climate variability and change and recruitment of juvenile fishes to adult populations is critical for understanding variability in stock–recruit dynamics. [2] In this presentation we will summarize results obtained during the first year of the project, the contribution of satellite measurements for monitoring SSS and the specific objectives of the CCI-SSS project: - a definition of the requirements for SSS ECV products relevant for the climate studies and consistent with the satellite SSS achievable performances - an harmonization of the SSS products and of the radiative transfer models for a long term consistent and stable SSS time series - a thorough characterization of the uncertainties of the SSS ECV , - an assessment of the ECV product through five case studies related to ocean climate variability and hydrological cycle - Exchange of knowledge between the CCI+SSS team and the international community. [3] Understanding and monitoring ocean climate variability and change, to constrain and initialize models as well as identify model biases for improved climate hindcasting and prediction, requires a scale-sensitive, and long-term observing system. [4] These indices were compared to the Pacific Decadal Oscillation (PDO), an index of Pacific Ocean climate variability. [5]

ocean climate state

With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea level, mostly due to increased model resolution and updates in assimilated observation data sets. [1] ARC3O is therefore capable to realistically translate the simulated Arctic Ocean climate state into one observable quantity for a more comprehensive climate model evaluation and initialization. [2] With respect to ORAS4, ORAS5 has improved ocean climate state and variability in terms of SST and sea-level, mostly due to increased model resolution and updates in assimilated observation data sets. [3]

ocean climate modeling

The ocean surface net radiation ( $R_{n}$ ) characterizing ocean surface radiation budget is a key variable in ocean climate modeling and analysis. [1] The ocean surface net radiation (Rn) characterizing the ocean surface radiation budget, is a key variable of interest in ocean climate modeling and analysis, which determines the climate model of ocean surface with heat, freshwater and momentum flux. [2]

ocean climate system

The Amery Ice Shelf (AIS) dynamics and mass balance caused by iceberg calving and basal melting are significant in the ocean climate system. [1] This period is too short to evaluate many fundamental aspects of the Antarctic and Southern Ocean climate system, such as decadal-to-century time-scale climate variability and trends. [2]