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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Sustainable development. ; Electronic books.
    Description / Table of Contents: This volume offers a survey and analysis of efforts to develop actionable climate information in support of vital decisions for climate adaptation, risk management and policy. It identifies research priorities from seasons to decades and longer time scales.
    Type of Medium: Online Resource
    Pages: 1 online resource (506 pages)
    Edition: 1st ed.
    ISBN: 9789400766921
    DDC: 333.714
    Language: English
    Note: Intro -- Contents -- List of Figures -- List of Tables -- Contributors -- The World Climate Research Program Strategy and Priorities: Next Decade -- 1 Introduction -- 2 Evolution of WCRP Research Mandate -- 3 Future Plans and Priorities of WCRP Major Sponsors -- 4 Overview of Following Chapters -- 5 Summary -- References -- Challenges of a Sustained Climate Observing System -- 1 Introduction -- 2 The Current Climate Observing System -- 2.1 Status of Systematic Climate Observations -- 2.2 Building a System for Climate Observations -- 2.3 Developing Operational Components -- 3 Lost in Space: Climate Observations? -- 3.1 Current and Programmed Satellite Observations -- 3.2 Adequacy of In-Situ Observations -- 3.3 The Scope of the Challenge of Satellite Observations: Adequacy and Issues -- 3.3.1 The Missing Satellite Observing System Principles -- 3.3.2 Delays and Cost Increases -- 3.4 Decadal Change Accuracy: Unbroken Chain of Uncertainty to SI Standards -- 3.4.1 Accuracy and SI Standards -- 3.4.2 Stability of Observations and Algorithms -- 3.4.3 Accuracy -- 3.5 Improving Transitions Between Observing Systems -- 3.6 How to Prioritize? -- 4 Analyses, Assessments and Reprocessing -- 4.1 Reanalyses -- 4.2 Assessments -- 5 Further Needed Improvements -- 5.1 In Situ Observations -- 5.2 Data Documentation and Adequacy of Metadata -- 5.3 Tracking Climate Observing Performance -- 5.4 Climate Observations at High Risk -- 6 Appendix A: The GCOS Organizational Framework -- References -- On the Reprocessing and Reanalysis of Observations for Climate -- 1 Reprocessing Observations -- 1.1 Data Recovery and Archiving -- 1.2 Data Set Creation and Evaluation -- 1.3 Recommendations -- 2 Reanalysis of Observations -- 2.1 Current Status -- 2.2 Integrating Earth System Analyses -- 2.3 Reanalysis Input Observations -- 2.4 Recommendations -- 3 Future Directions. , References -- Climate Processes: Clouds, Aerosols and Dynamics -- 1 Introduction -- 2 Recent Scientific Advances -- 2.1 Clouds and Convection -- 2.1.1 Boundary Layer Clouds and Dynamics -- 2.1.2 Deep Convection and Its Dynamical Coupling to Larger Scales -- 2.1.3 Microphysics -- 2.1.4 Trends, Variations and Feedbacks -- 2.2 Aerosols and Aerosol-Cloud Interactions -- 2.2.1 Sources, Ageing and Sinks of Aerosols in the Atmosphere -- 2.2.2 Direct and Indirect Radiative Effects of Aerosols on Climate -- 2.2.3 Microphysical Effects of Aerosols on Precipitation and Vice Versa -- 2.2.4 Advances in Parameterizing Aerosols -- 2.3 Dynamics from Small to Global Scales -- 2.3.1 Gravity Waves -- 2.3.2 Blocking Events -- 2.3.3 Widening of the Tropics -- 2.3.4 Impact of the Stratosphere on the Large-Scale Circulation -- 2.3.5 Impact of Warming on Rainfall Extremes, Cyclones, and Severe Storms -- 3 Current Scientific Gaps and Open Questions -- 3.1 Clouds and Convection -- 3.2 Aerosols and Aerosol-Cloud Interactions -- 3.3 Dynamics from Small to Global Scales -- 4 Strategic Opportunities and Recommendations -- 4.1 Research Foci, Strategies and Resources -- 4.1.1 Confront Two-Way Integration Across Scales -- 4.1.2 Emphasize Fundamental Science and Model Development -- 4.1.3 Explore Hierarchical Modeling Approaches -- 4.1.4 Integrate the Whole Atmosphere, Ocean and Surface -- 4.1.5 Plan for the High-Resolution Future -- 4.1.6 Bring Weather to Climate -- 4.1.7 Sustain and Improve Observations -- 4.2 Research Coordination -- 5 Summary -- References -- Aerosol Cloud-Mediated Radiative Forcing: Highly Uncertain and Opposite Effects from Shallow and Deep Clouds -- 1 Introduction -- 2 Aerosol-Induced Radiative Forcing by Boundary-Layer Warm Clouds -- 2.1 The Fundamental Physical Processes -- 2.2 Aerosol Effects on Non-precipitating and Modestly Precipitating Clouds. , 2.3 Aerosol Effects on the Transition to Precipitating Clouds -- 2.4 The Frequency of Occurrence of Aerosol-Starved Cloud Regimes -- 2.5 The Attribution of the Regime Changes to Anthropogenic Aerosols -- 2.6 The Possible Underestimation of the Radiative Forcing Via Low Clouds -- 3 Aerosol Induced Radiative Forcing by Deep Convective Clouds -- 3.1 Aerosol Invigoration of Deep Clouds in Warm and Moist Atmosphere -- 3.2 Aerosols Enhancing Detrainment of Ice and Vapor in the UTLS -- 4 Aerosol Induced Radiative Forcing by Supercooled Layer Clouds -- 5 Discussion and Implications for GCMs -- 6 What Should We Do Next? -- 7 Summary -- References -- Improving Understanding of the Global Hydrologic Cycle -- 1 Introduction: The Challenge -- 2 Current WCRP Efforts -- 3 Improve Collection of Hydrological and Water System Data -- 3.1 Ground-Based, In-Situ Observations -- 3.2 Remotely Sensed Observations -- 3.3 Managing Data -- 4 Modeling -- 5 Hydrological Sciences Needs for the Twenty-First Century in the Earth System Context -- 5.1 Climate, Water, and Social Adaptation -- 5.2 Water, Energy, Agricultural Nexus -- 5.3 Water Quality and Ecosystems -- 6 A Grand Challenge in Hydrologic and Water-Resources Modeling -- 7 Conclusions -- References -- Land Use and Land Cover Changes and Their Impacts on Hydroclimate, Ecosystems and Society -- 1 Introduction -- 2 Land Use Change and Hydroclimate -- 3 Land Use Change and Ecosystems -- 4 Societal Needs for Research on Water Over Land -- 5 Current Gaps, and Future Challenges -- 6 Concluding Remarks -- References -- Prediction from Weeks to Decades -- 1 Introduction -- 2 Sub-seasonal Prediction -- 2.1 Madden Julian Oscillation -- 2.2 Other Sources of Sub-seasonal Predictability -- 3 Seasonal-to-Interannual Prediction -- 3.1 El Nino Southern Oscillation (ENSO) -- 3.2 Tropical Atlantic Variability. , 3.3 Tropical Indian Ocean Variability -- 3.4 Other Sources of Seasonal to Interannual Predictability -- 3.4.1 Upper Ocean Heat Content -- 3.4.2 Snow Cover -- 3.4.3 Stratosphere -- 3.4.4 Vegetation and Land Use -- 3.4.5 Polar Sea Ice -- 4 Decadal Prediction -- 4.1 Potential Sources of Decadal Predictability -- 4.1.1 External Forcing -- 4.1.2 Atlantic Multi-decadal Variability -- 4.1.3 Pacific Decadal Variability -- 4.1.4 Other Sources of Decadal Predictability -- 4.2 Achievements So Far -- 5 Summary -- 5.1 Improving the Fidelity of the Climate Models at the Heart of Forecast Systems -- 5.2 Developing More Sophisticated Measures of Defining and Verifying Forecast Reliability and Skill for the Different Lead Times -- 5.3 Design of Ensemble Prediction Systems -- 5.4 Utility of Monthly to Decadal Predictions -- References -- Assessing the Reliability of Climate Models, CMIP5 -- 1 Introduction -- 2 The Implications (and Usefulness) of Model Spread -- 3 New Observations and Diagnostics -- 4 Examples of Process Evaluations Currently in Progress -- 5 Summary and Recommendations for WCRP -- References -- Changes in Variability Associated with Climate Change -- 1 Introduction -- 2 How Do Changes in Greenhouse Gases and Solar and Orbital Parameters Impact the Tropics? -- 2.1 ENSO -- 2.2 Width of the Tropics -- 3 How Does Climate Change Impact Middle and High Latitudes? -- 3.1 The Northern Annular Mode and Related Latitudinal Shifts of the Eddy-Driven Jet -- 3.2 The Southern Annular Mode -- 3.3 Sea Ice and Associated Atmospheric and Oceanic Circulations -- 4 How Do Greenhouse Gas Induced Climate Changes Interact with Ozone Depletion? -- 5 Summary -- References -- Understanding and Predicting Climate Variability and Change at Monsoon Regions -- 1 Introduction -- 2 Regional Perspectives -- 2.1 Asian-Australian Monsoons. , 2.1.1 Regional Variability and Predictability -- 2.1.2 Long-Term Trends and Projections -- 2.2 American Monsoon Systems -- 2.2.1 Regional Variability and Predictability -- 2.2.2 Long-Term Trends and Projections -- 2.3 Sub-Saharan Africa -- 2.3.1 Regional Variability and Predictability -- 2.3.2 Long-Term Trends and Projections -- 3 Regional Climate Simulation -- 3.1 Regionalization Needs -- 3.2 Coordinated Downscaling Exercises -- 4 Challenges in Monsoon Simulation and Prediction -- 4.1 Large to Regional Scale Processes Influencing Monsoon Variability and Predictability -- 4.2 Key Local to Regional Processes Influencing Monsoon Variability and Predictability -- 4.2.1 Surface Heterogeneity -- 4.2.2 Diurnal Cycle -- 4.2.3 Low Level Jets -- 4.2.4 Regional Ocean-Atmosphere Coupling -- 5 Challenges in Generating Actionable Regional Climate Information -- 6 Concluding Remarks -- References -- Attribution of Weather and Climate-Related Events -- 1 Introduction -- 2 Relevance of Attribution Assessments of Weather and Climate-Related Events -- 2.1 Improved Climate Science -- 2.2 General Public -- 2.3 Litigation -- 2.4 Adaptation -- 2.5 Geoengineering -- 2.6 Insurance -- 3 Development of Event Attribution -- 4 Examples of Event Attribution for Specific Cases -- 4.1 2003 Central European Summer Temperatures -- 4.2 2000 UK Floods -- 4.3 2008 Cool US -- 4.4 2010 Russian Heatwave -- 5 Attribution of Climate-Related Events Group -- 6 Development of Near-Real Time Weather and Climate Event Attribution -- 6.1 Coupled Model Approaches -- 6.2 Very Large Ensembles Using Distributed Computing Experiments -- 6.3 Analogue Methods for Diagnosing the Influence of Circulation Characteristics -- 6.4 A Near-Real Time Attribution Capability Linked to Seasonal Forecasting -- 7 Discussion: Lessons Learned and Future Research Needs -- References. , Climate Extremes: Challenges in Estimating and Understanding Recent Changes in the Frequency and Intensity of Extreme Climate and Weather Events.
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  • 2
    Online Resource
    Online Resource
    Oxford :Oxford University Press, Incorporated,
    Keywords: Marine ecology -- North Atlantic Ocean. ; Climatic changes -- Environmental aspects -- North Atlantic Ocean. ; Marine animals -- Climatic factors. ; North Atlantic Ocean -- Climate. ; Electronic books.
    Description / Table of Contents: This research level text focuses on the influence of climate variability on the marine ecosystems of the North Atlantic. The ecological impact of climate variability on population dynamics is addressed at the full range of trophic levels, from phytoplankton through zooplankton and fish to marine birds. Climate effects on biodiversity and community structure are also examined. Forty scientists from around the world synthesize what is currently known about how climateaffects the ecological systems of the North Atlantic and then place these insights within a broader ecological perspective. Many of the general features of the North Atlantic region are also seen in other marine ecosystems as well as terrestrial and freshwater systems. The final section of the bookmakes these generalities more explicit, so as to stimulate communication and promote co-operation amongst researchers who may previously have worked in semi-isolation.
    Type of Medium: Online Resource
    Pages: 1 online resource (267 pages)
    Edition: 1st ed.
    ISBN: 9780191523168
    DDC: 577.7/22/091631;577.731
    Language: English
    Note: Intro -- Contents -- Contributors -- Acronym list -- North Atlantic Region Map -- PART I: Background to climate variation and its effects on marine ecology -- 1 Climatic fluctuations and marine systems: a general introduction to the ecological effects -- 2 Climate variability over the North Atlantic -- 3 Modelling marine ecosystems and their environmental forcing -- PART II: Plankton populations -- 4 Responses of marine phytoplankton populations to fluctuations in marine climate -- 5 The influences of climate variability on North Atlantic zooplankton populations -- PART III: Fish and seabird populations -- 6 The responses of fish populations to ocean climate fluctuations -- 7 Marine birds and climate fluctuation in the North Atlantic -- PART IV: Community ecology -- 8 Responses of phytoplankton communities to climate variability -- 9 Effects of climate variability on benthic communities -- 10 Climatic influences on marine fish community ecology -- PART V: Climate impacts on North Atlantic marine ecology-views from outside -- 11 Climate and fisheries: an insight from the Central Pacific Ocean -- 12 Complexity of marine fisheries dynamics and climate interactions in the northeast Pacific Ocean -- 13 A fresh (water) perspective on the impacts of the NAO on North Atlantic ecology -- 14 A freshwater perspective on climate variability and its effect on marine ecosystems -- 15 Time lags in terrestrial and marine environments -- 16 The impacts of ENSO on terrestrial ecosystems: a comparison with NAO -- PART VI: Conclusion-what are the ecological effects of climate variation in the North Atlantic? -- Afterword -- References -- Glossary of Species Names -- A -- B -- C -- D -- E -- F -- G -- H -- J -- L -- M -- N -- O -- P -- R -- S -- T -- W -- Y -- Index -- A -- B -- C -- D -- E -- F -- G -- H -- I -- J -- K -- L -- M -- N -- O -- P -- Q -- R -- S -- T. , U -- V -- W -- Y -- Z -- Subject Index -- A -- B -- C -- D -- E -- F -- G -- H -- I -- J -- K -- L -- M -- N -- O -- P -- R -- S -- T -- U -- V -- W -- Y -- Z.
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  • 3
    Book
    Book
    Washington, D.C. : American Geophysical Union
    Keywords: North Atlantic oscillation Environmental aspects ; Atmospheric circulation North Atlantic Ocean ; North Atlantic oscillation Environmental aspects ; Atmospheric circulation North Atlantic Ocean ; North Atlantic Ocean Climate ; North Atlantic Ocean Climate ; Aufsatzsammlung ; Atlantischer Ozean Nord ; Allgemeine atmosphärische Zirkulation
    Type of Medium: Book
    Pages: VIII, 279 S. , graph. Darst., Kt.
    ISBN: 0875909949
    Series Statement: Geophysical monograph series 134
    DDC: 551.524633
    RVK:
    RVK:
    Language: English
    Note: Includes bibliographical references , Includes bibliographical references
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 386 (1997), S. 164-167 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The relative merits of the surface and MSU temperature records have been a matter of spirited debate1. One often overlooked issue is that there is no single satellite record, and that different tropospheric measures of temperature from the MSUs contain different trends and different error ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 11 (1995), S. 25-50 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract.  The simulated mean January and July climates of four versions of the National Center for Atmospheric Research (NCAR) Community Climate Model (CCM) are compared. The models include standard configurations of CCM1 and CCM2, as well as two widely-cited research versions, the Global Environmental and Ecological Simulation of Interactive Systems (GENESIS) model and the Climate Sensitivity and Carbon Dioxide (CSCO2) model. Each CCM version was integrated for 10 years with a horizontal spectral resolution of rhomboidal 15 (R15). Additionally, the standard T42 version of CCM2 was integrated for 20 years. Monthly mean, annually repeating climatological sea surface temperatures provided a lower boundary condition for each of the model simulations. The CCM troposphere is generally too cold, especially in the polar upper troposphere in the summer hemisphere. This is least severe in CCM2 and most pronounced in CCM1. CSCO2 is an exception with a substantial warm bias, especially in the tropical upper troposphere. Corresponding biases are evident in atmospheric moisture. The overall superior CCM2 thermodynamic behavior is principally compromised by a large warm and moist bias over the Northern Hemisphere middle and high latitudes during summer. Differences between the simulated and observed stationary wave patterns reveal sizeable amplitude errors and phase shifts in all CCM versions. A common problem evident in the upper troposphere is an erroneous cyclone pair that straddles the equatorial central Pacific in January. The overall January stationary wave error pattern in CCM2 and CSCO2 is suggestive of a reverse Pacific-North American teleconnection pattern originating from the tropical central Pacific. During July, common regional biases include simulated North Pacific troughs that are stronger and shifted to the west of observations, and each model overestimates the strength of the anticyclone pair associated with the summer monsoon circulation over India. The simulated major convergence and divergence centers tend to be very localized in all CCM versions, with a tendency in each model for the maximum divergent centers to be unrelistically concentrated in monsoon regions and tied to regions of steep orography. Maxima in CCM-simulated precipitation correspond to the simulated outflow maxima and are generally larger than observational estimates, and the associated atmospheric latent heating appears to contribute to the stationary wave errors. Comparisons of simulated radiative quantities to satellite measurements reveal that the overall CCM2 radiative balance is better than in the other CCM versions. An error common to all models is that too much solar radiation is absorbed in the middle latitudes during summer.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 11 (1995), S. 25-50 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The simulated mean January and July climates of four versions of the National Center for Atmospheric Research (NCAR) Community Climate Model (CCM) are compared. The models include standard configurations of CCM1 and CCM2, as well as two widely-cited research versions, the Global Environmental and Ecological Simulation of Interactive Systems (GENESIS) model and the Climate Sensitivity and Carbon Dioxide (CSC02) model. Each CCM version was integrated for 10 years with a horizontal spectral resolution of rhomboidal 15 (R15). Additionally, the standard T42 version of CCM2 was integrated for 20 years. Monthly mean, annually repeating climatological sea surface temperatures provided a lower boundary condition for each of the model simulations. The CCM troposphere is generally too cold, especially in the polar upper troposphere in the summer hemisphere. This is least severe in CCM2 and most pronounced in CCM1. CSC02 is an exception with a substantial warm bias, especially in the tropical upper troposphere. Corresponding biases are evident in atmospheric moisture. The overall superior CCM2 thermodynamic behavior is principally compromised by a large warm and moist bias over the Northern Hemisphere middle and high latitudes during summer. Differences between the simulated and observed stationary wave patterns reveal sizeable amplitude errors and phase shifts in all CCM versions. A common problem evident in the upper troposphere is an erroneous cyclone pair that straddles the equatorial central Pacific in January. The overall January stationary wave error pattern in CCM2 and CSCO2 is suggestive of a reverse Pacific-North American teleconnection pattern originating from the tropical central Pacific. During July, common regional biases include simulated North Pacific troughs that are stronger and shifted to the west of observations, and each model overestimates the strength of the anticyclone pair associated with the summer monsoon circulation over India. The simulated major convergence and divergence centers tend to be very localized in all CCM versions, with a tendency in each model for the maximum divergent centers to be unrelistically concentrated in monsoon regions and tied to regions of steep orography. Maxima in CCM-simulated precipitation correspond to the simulated outflow maxima and are generally larger than observational estimates, and the associated atmospheric latent heating appears to contribute to the stationary wave errors. Comparisons of simulated radiative quantities to satellite measurements reveal that the overall CCM2 radiative balance is better than in the other CCM versions. An error common to all models is that too much solar radiation is absorbed in the middle latitudes during summer.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 9 (1994), S. 303-319 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract. Considerable evidence has emerged of a substantial decade-long change in the north Pacific atmosphere and ocean lasting from about 1976 to 1988. Observed significant changes in the atmospheric circulation throughout the troposphere revealed a deeper and eastward shifted Aleutian low pressure system in the winter half year which advected warmer and moister air along the west coast of North America and into Alaska and colder air over the north Pacific. Consequently, there were increases in temperatures and sea surface temperatures (SSTs) along the west coast of North America and Alaska but decreases in SSTs over the central north Pacific, as well as changes in coastal rainfall and streamflow, and decreases in sea ice in the Bering Sea. Associated changes occurred in the surface wind stress, and, by inference, in the Sverdrup transport in the north Pacific Ocean. Changes in the monthly mean flow were accompanied by a southward shift in the storm tracks and associated synoptic eddy activity and in the surface ocean sensible and latent heat fluxes. In addition to the changes in the physical environment, the deeper Aleutian low increased the nutrient supply as seen through increases in total chlorophyll in the water column, phytoplankton and zooplankton. These changes, along with the altered ocean currents and temperatures, changed the migration patterns and increased the stock of many fish species. A north Pacific (NP) index is defined to measure the decadal variations, and the temporal variability of the index is explored on daily, annual, interannual and decadal time scales. The dominant atmosphere-ocean relation in the north Pacific is one where atmospheric changes lead SSTs by one to two months. However, strong ties are revealed with events in the tropical Pacific, with changes in tropical Pacific SSTs leading SSTs in the north Pacific by three months. Changes in the storm tracks in the north Pacific help to reinforce and maintain the anomalous circulation in the upper troposphere. A hypothesis is put forward outlining the tropical and extratropical realtionships which stresses the role of tropical forcing but with important feedbacks in the extratropics that serve to emphasize the decadal relative to interannual time scales. The Pacific decadal timescale variations are linked to recent changes in the frequency and intensity of El Niño versus La Niña events but whether climate change associated with ”global warming" is a factor is an open question.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 9 (1994), S. 303-319 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Considerable evidence has emerged of a substantial decade-long change in the north Pacific atmosphere and ocean lasting from about 1976 to 1988. Observed significant changes in the atmospheric circulation throughout the troposphere revealed a deeper and eastward shifted Aleutian low pressure system in the winter half year which advected warmer and moister air along the west coast of North America and into Alaska and colder air over the north Pacific. Consequently, there were increases in temperatures and sea surface temperatures (SSTs) along the west coast of North America and Alaska but decreases in SSTs over the central north Pacific, as well as changes in coastal rainfall and streamflow, and decreases in sea ice in the Bering Sea. Associated changes occurred in the surface wind stress, and, by inference, in the Sverdrup transport in the north Pacific Ocean. Changes in the monthly mean flow were accompanied by a southward shift in the storm tracks and associated synoptic eddy activity and in the surface ocean sensible and latent heat fluxes. In addition to the changes in the physical environment, the deeper Aleutian low increased the nutrient supply as seen through increases in total chlorophyll in the water column, phytoplankton and zooplankton. These changes, along with the altered ocean currents and temperatures, changed the migration patterns and increased the stock of many fish species. A north Pacific (NP) index is defined to measure the decadal variations, and the temporal variability of the index is explored on daily, annual, interannual and decadal time scales. The dominant atmosphere-ocean relation in the north Pacific is one where atmospheric changes lead SSTs by one to two months. However, strong ties are revealed with events in the tropical Pacific, with changes in tropical Pacific SSTs leading SSTs in the north Pacific by three months. Changes in the storm tracks in the north Pacific help to reinforce and maintain the anomalous circulation in the upper troposphere. A hypothesis is put forward outlining the tropical and extratropical realtionships which stresses the role of tropical forcing but with important feed-backs in the extratropics that serve to emphasize the decadal relative to interannual time scales. The Pacific decadal timescale variations are linked to recent changes in the frequency and intensity of El Niño versus La Nina events but whether climate change associated with “global warming” is a factor is an open question.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 36 (1997), S. 301-326 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Large changes in the wintertime atmospheric circulation have occurred over the past two decades over the ocean basins of the Northern Hemisphere, and these changes have had a profound effect on regional distributions of surface temperature and precipitation. The changes over the North Pacific have been well documented and have contributed to increases in temperatures across Alaska and much of western North America and to decreases in sea surface temperatures over the central North Pacific. The variations over the North Atlantic are related to changes in the North Atlantic Oscillation (NAO). Over the past 130 years, the NAO has exhibited considerable variability at quasi-biennial and quasi-decadal time scales, and the latter have become especially pronounced the second half of this century. Since 1980, the NAO has tended to remain in one extreme phase and has accounted for a substantial part of the observed wintertime surface warming over Europe and downstream over Eurasia and cooling in the northwest Atlantic. Anomalies in precipitation, including dry wintertime conditions over southern Europe and the Mediterranean and wetter-than-normal conditions over northern Europe and Scandinavia since 1980, are also linked to the behavior of the NAO. Changes in the monthly mean flow over the Atlantic are accompanied by a northward shift in the storm tracks and associated synoptic eddy activity, and these changes help to reinforce and maintain the anomalous mean circulation in the upper troposphere. It is important that studies of trends in local climate records, such as those from high elevation sites, recognize the presence of strong regional patterns of change associated with phenomena like the NAO.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2012. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Climate 25 (2012): 5153–5172, doi:10.1175/JCLI-D-11-00463.1.
    Description: Atlantic meridional overturning circulation (AMOC) variability is documented in the Community Climate System Model, version 4 (CCSM4) preindustrial control simulation that uses nominal 1° horizontal resolution in all its components. AMOC shows a broad spectrum of low-frequency variability covering the 50–200-yr range, contrasting sharply with the multidecadal variability seen in the T85 × 1 resolution CCSM3 present-day control simulation. Furthermore, the amplitude of variability is much reduced in CCSM4 compared to that of CCSM3. Similarities as well as differences in AMOC variability mechanisms between CCSM3 and CCSM4 are discussed. As in CCSM3, the CCSM4 AMOC variability is primarily driven by the positive density anomalies at the Labrador Sea (LS) deep-water formation site, peaking 2 yr prior to an AMOC maximum. All processes, including parameterized mesoscale and submesoscale eddies, play a role in the creation of salinity anomalies that dominate these density anomalies. High Nordic Sea densities do not necessarily lead to increased overflow transports because the overflow physics is governed by source and interior region density differences. Increased overflow transports do not lead to a higher AMOC either but instead appear to be a precursor to lower AMOC transports through enhanced stratification in LS. This has important implications for decadal prediction studies. The North Atlantic Oscillation (NAO) is significantly correlated with the positive boundary layer depth and density anomalies prior to an AMOC maximum. This suggests a role for NAO through setting the surface flux anomalies in LS and affecting the subpolar gyre circulation strength.
    Description: The CCSM project is supported by NSF and the Office of Science (BER) of the U.S. Department of Energy. SGY and YOK were supported by the NOAA Climate Program Office under Climate Variability and Predictability Program Grants NA09OAR4310163 and NA10OAR4310202, respectively.
    Description: 2013-02-01
    Keywords: Meridional overturning circulation ; Coupled models ; Ocean models ; Oceanic variability
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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