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  • 2020-2024  (18)
  • 1955-1959  (41)
  • 1935-1939  (14)
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  • 1
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    Springer Nature | Springer Nature Singapore
    Publication Date: 2024-03-29
    Description: This open access book consists of essays selected from Joseph S. Nye, Jr.’s last three decades of writing and illustrate a variety of perspectives on the nature of power, the role of the United States in the world and US-China relations. Through this collection, it is hoped that readers will gain a better understanding of today’s global environment and find that while great power competition may be inevitable in a world as centers of power shift, cooperating to address transnational challenges can be a positive sum game. The contents of this book are divided into four main parts. Part One discusses the origins and political progress of the concept of “Soft Power”. Part Two explores soft power in the American experience, its sources and interaction with US foreign policy, as well as its ebb and flow in the age of Obama, Trump and Biden. Part Three examines the rise of and the opportunities and difficulties for Chinese soft power, focusing on China’s investment in soft power and how this demonstrates its commitment to a peaceful rise. However, it also addresses the question of how can China get “smart” on how it uses soft power. Part Four provides a bird’s-eye view of power shifts in the 21st century and the interactions between the US as an established power and China as a rising power, while also reassuring readers that Thucydidean fears are unnecessary and a Cold War is avoidable. Both countries have to realize that some forms of power must be exercised with others, not over others, the development of soft power need not be a zero-sum game. Ultimately, the US-China relationship is a “cooperative rivalry” where a successful strategy of “smart competition” is necessary and cooperation on transnational challenges like climate change, pandemics, cyberterrorism and nuclear proliferation, will serve to benefit not only China and the US, but the world as a whole.
    Keywords: Soft Power ; US-China Relations ; China Rising ; Smart Power ; Nye Report ; The Kindleberger Trap ; Cooperative Rivalry ; Interdependence ; Liberal International Order ; Moral Foreign Policy ; thema EDItEUR::J Society and Social Sciences::JP Politics and government::JPS International relations ; thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GT Interdisciplinary studies::GTQ Globalization
    Language: English
    Format: image/jpeg
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  • 2
    Publication Date: 2023-07-19
    Keywords: Comment; Conductivity, thermal; DATE/TIME; DEPTH, soil; Description; Goodness of fit; Heat capacity, volumetric; land-air exchange; LATITUDE; Location; LONGITUDE; Permafrost; polar desert; Resistivity, thermal; Sample ID; Sensor type; soil hydrology; surface energy balance; Taylor_valley; Thermal diffusivity; Transantarctic Mountains; water track
    Type: Dataset
    Format: text/tab-separated-values, 385 data points
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  • 3
    Publication Date: 2024-05-18
    Description: The data comprise meters composite depth (mcd) versus component declination, inclination and maximum angular deviation (MAD) values for natural remanent magnetization (NRM) from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. The component magnetizations were determined from stepwise alternating field demagnetization of NRM and measured on a pass-through u-channel magnetometer (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and relative paleointensity (RPI) data are used in tandem to generate an age model for the last 1 Myr. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305.
    Keywords: 303-U1306; COMPCORE; Composite Core; Declination; Deep Western Boundary Current; DEPTH, sediment/rock; Eirik Drift; Exp303; Inclination; Joides Resolution; Maximum angular deviation; North Atlantic; North Atlantic Climate 1; Northwest Atlantic; Oxygen isotopes; Quaternary; relative paleointensity; see Channell et al. (2014)
    Type: Dataset
    Format: text/tab-separated-values, 61119 data points
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  • 4
    Publication Date: 2024-05-18
    Description: The data comprise meters composite depth (mcd) versus volume susceptibility (x10-3 SI) and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. The anhysteretic magnetization (ARM) was measured on a pass-through u-channel magnetometer and the volume susceptibilities were measured on a pass-through (u-channel) susceptibility bridge (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and relative paleointensity (RPI) data are used in tandem to generate an age model for the last 1 Myr from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305.
    Keywords: 303-U1306; Anhysteretic susceptibility/magnetic susceptibility; COMPCORE; Composite Core; Deep Western Boundary Current; DEPTH, sediment/rock; Eirik Drift; Exp303; Joides Resolution; Magnetic susceptibility, volume; North Atlantic; North Atlantic Climate 1; Northwest Atlantic; Oxygen isotopes; Quaternary; relative paleointensity; see Channell et al. (2014)
    Type: Dataset
    Format: text/tab-separated-values, 40746 data points
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  • 5
    Publication Date: 2024-05-18
    Description: The data comprise meters composite depth (mcd) versus oxygen isotope measurements on Neogloboquadrina pachyderma from Integrated Ocean Drilling Program (IODP) Site U130 using a Fisons Optima mass spectrometer at Rutgers University (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and relative paleointensity (RPI) data are used in tandem to generate an age model for the last 1 Myr from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305.
    Keywords: 303-U1306; COMPCORE; Composite Core; Deep Western Boundary Current; DEPTH, sediment/rock; Eirik Drift; Exp303; Joides Resolution; Mass spectrometer Fisons Optima; Neogloboquadrina pachyderma, δ18O; North Atlantic; North Atlantic Climate 1; Northwest Atlantic; Oxygen isotopes; Quaternary; relative paleointensity
    Type: Dataset
    Format: text/tab-separated-values, 2710 data points
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  • 6
    Publication Date: 2024-05-18
    Description: The data comprise meters composite depth (mcd) versus a relative paleointensity (RPI) proxy from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. The RPI proxy is natural remanent magnetization (NRM) normalized by anhysteretic remanent magnetization (ARM). The NRM/ARM paleointensity proxy was calculated as a slope over the 20-60 mT peak field demagnetization range. Also listed are the correlation coefficients (r) representing the definition of the slopes. NRM and ARM were measured on a pass-through u-channel magnetometer (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and RPI data are used in tandem to generate an age model for the last 1 Myr from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305.
    Keywords: 303-U1306; Calculated; COMPCORE; Composite Core; Correlation coefficient; Deep Western Boundary Current; DEPTH, sediment/rock; Eirik Drift; Exp303; Joides Resolution; Natural remanent magnetization/anhysteretic remanent magnetization ratio; North Atlantic; North Atlantic Climate 1; Northwest Atlantic; Oxygen isotopes; Quaternary; relative paleointensity; see Channell et al. (2014)
    Type: Dataset
    Format: text/tab-separated-values, 40746 data points
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  • 7
    Publication Date: 2024-05-18
    Description: Sedimentary magnetic data along the revised stratigraphic splice from IODP Site U1396. The dataset includes the meters composite depth scale, three age models, and sedimentation rate. Sediment classification is from the shipboard data. Rock magnetic properties (MS, karm, karm/k, MDFarm) and paleomagnetic properties (optimized ChRM inclination, inclination anomaly, optimized ChRM declination, VGP Latitude, MAD values) are provided for every cm along the splice. NRM/ARMslope values provide a proxy for RPI and are presented with the R-value following filtering as outlined in the associated publication.
    Keywords: 2G u-channel SRM; 340-U1396A; 340-U1396B; 340-U1396C; Age model; Age model, GPTS (geomagnetic polarity timescale), Cande and Kent (1995); Age Model (Hatfield et al. 2021); Anhysteretic susceptibility; Anhysteretic susceptibility/magnetic susceptibility; ARM, median destructive field of anhysteretic remanent magnetization; Bartington MS2C sensor; ChRM, Declination; ChRM, Inclination; Core section label; Depth, composite; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp340; Inclination; Inclination Anomoly; Joides Resolution; Latitude of event; Lesser Antilles Volcanism and Landslides; Longitude of event; Magnetic Susceptibility, volumetric; Maximum angular deviation; Natural remanent magnetization/anhysteretic remanent magnetization ratio; Paleomagnetic data; Pliocene stratigraphy; rock magnetism; RPI data; Sample code/label; Section position; Sedimentary magnetism; Sedimentation rate; Sediment Classification; see Hatfield et al. (2021); Tephra; Virtual geomagnetic pole latitude
    Type: Dataset
    Format: text/tab-separated-values, 326310 data points
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  • 8
    Publication Date: 2024-05-29
    Keywords: 1st rotation angle (horizontal); 2nd rotation angle (vertical); Albedo, fraction; Battery terminal voltage; Buoyancy, flux; Carbon dioxide; Carbon dioxide, flux; Comment; Coriolis parameter f; Covariance; DATE/TIME; Date/time end; Date/time start; Day-Night indicator; Day of the year; Density, air; Density correction; Density of moist air; DEPTH, soil; Deviation; Device temperature net radiometer; Dew/frost point; Downward radiation, total; ELEVATION; Friction velocity; Ground heat, flux; Heat, flux, latent; Heat, flux, sensible; Heat, flux coefficient; Heat storage change; Height; Humidity, relative; Indicator; Integral turbulence characteristic; Kurtosis; land-air exchange; Latent heat of vaporization; LATITUDE; LONGITUDE; Long-wave downward radiation; Long-wave net radiation; Long-wave upward radiation; Momentum, flux; Net radiation; Non-stationarity; Number; Number of data; Number of measurements; Obukhov length; Percentage; Permafrost; polar desert; Pressure; Quality flag; Short-wave downward (GLOBAL) radiation; Short-wave net radiation; Short-wave upward (REFLEX) radiation; Skewness; Soil heat, flux; soil hydrology; Solar azimuth angle; Solar zenith angle; Sonic temperature; Specific heat, air; Spectral frequency correction factor; Standard deviation; surface energy balance; Taylor_valley; Temperature, air; Temperature, soil; Temperature, technical; Time lag; Transantarctic Mountains; Turbulence intensity; Upward radiation, total; UTC offset; Vapour pressure; Vapour saturation pressure; water track; Water vapour; Wind direction; Wind speed, along-wind, rotated, mean; Wind speed, cross-wind, rotated, mean; Wind speed, vertical, rotated, mean; Wind speed, x component; Wind speed, y component; Wind speed, z component; zeta
    Type: Dataset
    Format: text/tab-separated-values, 208994 data points
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  • 9
    Publication Date: 2024-05-29
    Keywords: 1st rotation angle (horizontal); 2nd rotation angle (vertical); Albedo, fraction; Battery terminal voltage; Buoyancy, flux; Carbon dioxide; Carbon dioxide, flux; Comment; Coriolis parameter f; Covariance; DATE/TIME; Date/time end; Date/time start; Day-Night indicator; Day of the year; Density, air; Density correction; Density of moist air; DEPTH, soil; Deviation; Device temperature net radiometer; Dew/frost point; Downward radiation, total; ELEVATION; Friction velocity; Ground heat, flux; Heat, flux, latent; Heat, flux, sensible; Heat, flux coefficient; Heat storage change; Height; Humidity, relative; Indicator; Integral turbulence characteristic; Kurtosis; land-air exchange; Latent heat of vaporization; LATITUDE; LONGITUDE; Long-wave downward radiation; Long-wave net radiation; Long-wave upward radiation; Momentum, flux; Net radiation; Non-stationarity; Number; Number of data; Number of measurements; Obukhov length; Permafrost; polar desert; Pressure; Quality flag; Short-wave downward (GLOBAL) radiation; Short-wave net radiation; Short-wave upward (REFLEX) radiation; Skewness; Soil heat, flux; soil hydrology; Solar azimuth angle; Solar zenith angle; Sonic temperature; Specific heat, air; Spectral frequency correction factor; Standard deviation; surface energy balance; Taylor_valley; Temperature, air; Temperature, soil; Temperature, technical; Time lag; Transantarctic Mountains; Turbulence intensity; Turbulence kinetic energy; Turbulence transport term; Upward radiation, total; UTC offset; Vapour pressure; Vapour saturation pressure; water track; Water vapour; Wind, along-wind component, scalar; Wind direction; Wind speed, along-wind, rotated, mean; Wind speed, cross-wind, rotated, mean; Wind speed, horizontal, scalar; Wind speed, total, scalar; Wind speed, vertical, rotated, mean; Wind speed, x component; Wind speed, y component; Wind speed, z component; zeta
    Type: Dataset
    Format: text/tab-separated-values, 205832 data points
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  • 10
    Publication Date: 2024-06-12
    Keywords: 341-U1417; AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; Exp341; Gulf of Alaska; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mid Pleistocene Transition; Size fraction 2.000-0.630 mm, coarse sand; Southern Alaska Margin: Tectonics, Climate and Sedimentation
    Type: Dataset
    Format: text/tab-separated-values, 360 data points
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