Space Physics Interactive Data Resource—SPIDR   总被引：1，自引：0，他引：1  

Mikhail Zhizhin  Eric Kihn  Rob Redmon  Dmitry Medvedev  Dmitry Mishin 《Earth Science Informatics》2008,1(2):79-91

SPIDR (Space Physics Interactive Data Resource) is a standard data source for solar-terrestrial physics, functioning within the framework of the ICSU World Data Centers. It is a distributed database and application server network, built to select, visualize and model historical space weather data distributed across the Internet. SPIDR can work as a fully-functional web-application (portal) or as a grid of web-services, providing functions for other applications to access its data holdings.

Mikhail ZhizhinEmail:

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Quantifying the effectiveness of climate change mitigation through forest plantations and carbon sequestration with an integrated land-use model     

Jelle G van Minnen  Bart J Strengers  Bas Eickhout  Rob J Swart  Rik Leemans 《Carbon balance and management》2008,3(1):1-20

Background

Carbon plantations are introduced in climate change policy as an option to slow the build-up of atmospheric carbon dioxide (CO₂) concentrations. Here we present a methodology to evaluate the potential effectiveness of carbon plantations. The methodology explicitly considers future long-term land-use change around the world and all relevant carbon (C) fluxes, including all natural fluxes. Both issues have generally been ignored in earlier studies.

Results

Two different baseline scenarios up to 2100 indicate that uncertainties in future land-use change lead to a near 100% difference in estimates of carbon sequestration potentials. Moreover, social, economic and institutional barriers preventing carbon plantations in natural vegetation areas decrease the physical potential by 75–80% or more. Nevertheless, carbon plantations can still considerably contribute to slowing the increase in the atmospheric CO₂ concentration but only in the long term. The most conservative set of assumptions lowers the increase of the atmospheric CO₂ concentration in 2100 by a 27 ppm and compensates for 5–7% of the total energy-related CO₂ emissions. The net sequestration up to 2020 is limited, given the short-term increased need for agricultural land in most regions and the long period needed to compensate for emissions through the establishment of the plantations. The potential is highest in the tropics, despite projections that most of the agricultural expansion will be in these regions. Plantations in high latitudes as Northern Europe and Northern Russia should only be established if the objective to sequester carbon is combined with other activities.

Conclusion

Carbon sequestration in plantations can play an important role in mitigating the build-up of atmospheric CO₂. The actual magnitude depends on natural and management factors, social barriers, and the time frame considered. In addition, there are a number of ancillary benefits for local communities and the environment. Carbon plantations are, however, particularly effective in the long term. Furthermore, plantations do not offer the ultimate solution towards stabilizing CO₂ concentrations but should be part of a broader package of options with clear energy emission reduction measures.  相似文献   

Paleomagnetism of the Upper Silurian and Lower Devonian carbonates of New York State: evidence for secondary magnetizations residing in magnetite     

Christopher R. Scotese  Rob Van der Voo  Chad McCabe 《Physics of the Earth and Planetary Interiors》1982,30(4):385-395

Paleomagnetic directions for the Upper Silurian and Lower Devonian carbonates of the Helderberg escarpment (New York State) differ from expected Late Silurian and Early Devonian directions for cratonic North America. The mean direction (D = 165°, I = −10°; paleopole at 50°N 129°E) is similar to Late Carboniferous and Early Permian results. Negative fold tests, and a lack of reversals, suggest that the magnetization is secondary. However, low coercivities, low blocking temperatures, the thermomagnetic curves (T_C near 570°C) and the acquisition of isothermal remanent magnetizations all suggest that the remanence is carried by magnetite. If a detrital origin of these magnetites is assumed, the secondary nature of the remanence would argue for thermal resetting as a result of deep burial of the rocks. However, no evidence for such thermal resetting is seen in the alteration of conodonts. More likely perhaps is a chemical or thermochemical origin of the remanence; this would require the magnetites to be authigenic.  相似文献   

Minimum continental velocities with respect to the pole since the Archean     

Laura Ullrich  Rob Van Der Voo 《Tectonophysics》1981,74(1-2)

Paleomagnetic apparent polar wander paths provide a method for estimating minimum plate velocities which can be extended much further into the geologic past than can be estimated based on sea-floor magnetic anomalies. Minimum velocities can be determined from the rate of change of latitude as derived relative to a fixed pole. Such latitudinal velocities have been determined for the center of mass of the North American, Baltic, Siberian and African shields since the Archean. The results indicate that plate velocities in the past have at times easily exceeded those for present-day continents, and that they often were equivalent to present-day oceanic velocities, although there are peaks and troughs through time. North American velocities are significantly greater prior to one billion years ago than those of Siberia or Baltica.  相似文献   

Lessons from China: building technological capabilities for low carbon technology transfer and development     

Jim Watson  Rob Byrne  David Ockwell  Michele Stua 《Climatic change》2015,131(3):387-399

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Foreign policy ‘trilemmas’: understanding China's stance on international cap-and-trade     

Yitian Huang  Rob Bailis 《Climate Policy》2013,13(4):494-516

This article uses a policy analogy approach to explore China's attitude toward the possibility of global carbon market integration, including the development of a common cap-and-trade market for the global civil aviation industry. Like in other foreign policy domains, in international cap-and-trade, China faces a ‘trilemma’ between carbon market integration, state sovereignty and policy flexibility. By referring to how China has approached a comparable trilemma in foreign exchange policy making, we analyse China's possible stance on international cap-and-trade. We argue that China will prefer to gradually establish and strengthen, to a limited extent, intergovernmental governance mechanisms, which allow nation-states to prioritize sovereignty and policy flexibility in carbon trading policy making. In the conclusion we use this argument to explain China's responses to the carbon-trading initiatives of Australia, the EU, the International Civil Aviation Organization (ICAO), and the World Bank.

Policy relevance

The international community has reached a consensus on the use of market mechanisms for mitigating climate change. While opposing the EU's plan to include Chinese airlines in the EU Emissions Trading Scheme, China has started to co-explore with Australia the possibility of linking their carbon markets, and has adopted a supportive attitude toward the carbon trading initiatives led by the ICAO and the World Bank. Considering China's status as the largest emitting country of GHGs and its interdependence with major developed and developing countries, China's substantial participation would be crucial to the success of the global market-based efforts to reduce GHG emissions. This article presents an initial attempt to develop a better understanding of China's stance on international cap-and-trade.  相似文献   

Late orogenic, large-scale rotations in the Tien Shan and adjacent mobile belts in Kyrgyzstan and Kazakhstan   总被引：6，自引：1，他引：5  

Rob Van der Voo  Natalia M. Levashova  Ludmila I. Skrinnik  Taras V. Kara  Mikhail L. Bazhenov   《Tectonophysics》2006,426(3-4):335-360

Most of Kazakhstan belongs to the central part of the Eurasian Paleozoic mobile belts for which previously proposed tectonic scenarios have been rather disparate. Of particular interest is the origin of strongly curved Middle and Late Paleozoic volcanic belts of island-arc and Andean-arc affinities that dominate the structure of Kazakhstan. We undertook a paleomagnetic study of Carboniferous to Upper Permian volcanics and sediments from several localities in the Ili River basin between the Tien Shan and the Junggar–Alatau ranges in southeast Kazakhstan. Our main goal was to investigate the Permian kinematic evolution of these belts, particularly in terms of rotations about vertical axes, in the hope of deciphering the dynamics that played a role during the latest Paleozoic deformation in this area. This deformation, in turn, can then be related to the amalgamation of this area with Baltica, Siberia, and Tarim in the expanding Eurasian supercontinent. Thermal demagnetization revealed that most Permian rocks retained a pretilting and likely primary component, which is of reversed polarity at three localities and normal at the fourth. In contrast, most Carboniferous rocks are dominated by postfolding reversed overprints of probably “mid-Permian” age, whereas presumably primary components are isolated from a few sites at two localities. Mean inclinations of primary components generally agree with coeval reference values extrapolated from Baltica, whereas declinations from primary as well as secondary components are deflected counterclockwise (ccw) by up to  90°. Such ccw rotated directions have previously also been observed in other Tien Shan sampling areas and in the adjacent Tarim Block to the south. However, two other areas in Kazakhstan show clockwise (cw) rotations of Permian magnetization directions. One area is located in the Kendyktas block about 300 km to the west of the Ili River valley, and the other is found in the Chingiz Range, to the north of Lake Balkhash and about 400 km to the north of the Ili River valley. The timing of the ccw as well as cw rotations is clearly later than the disappearance of any marine basins from northern Tarim, the Tien Shan and eastern Kazakhstan, so that the rotations cannot be attributed to island-arc or Andean-margin plate settings — instead we attribute the rotations to large-scale, east–west (present-day coordinates), sinistral wrenching in an intracontinental setting, related to convergence between Siberia and Baltica, as recently proposed by Natal'in and Şengör [Natal'in, B.A., and Şengör, A.M.C., 2005. Late Palaeozoic to Triassic evolution of the Turan and Scythian platforms: the pre-history of the palaeo-Tethyan closure, Tectonophysics, 404, 175–202.]. Our previous work in the Chingiz and North Tien Shan areas on Ordovician and Silurian rocks suggested relative rotations of  180°, whereas the Permian declination differences are of the order of 90° between the two areas. Thus, we assume that about 50% of the total post-Ordovician rotations are of pre-Late Permian age, with the other half of Late Permian–earliest Mesozoic age. The pre-Late Permian rotations are likely related to oroclinal bending during plate boundary evolution in a supra-subduction setting, given the calc-alkaline character of nearly all of the pre-Late Permian volcanics in the strongly curved belts.  相似文献   

Introduction: Magnetism and site formation processes in archaeology—2     

Rob Sternberg 《Geoarchaeology》1999,14(5):375-375

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