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321.
Max Auerbach 《Aquatic Sciences - Research Across Boundaries》1932,6(1-2):1-30
Ohne Zusammenfassung 相似文献
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323.
Max Richter 《International Journal of Earth Sciences》1928,19(1):51-62
Ohne Zusammenfassung 相似文献
324.
Takuji Waseda Leland Jameson Humio Mitsudera Max Yaremchuk 《Journal of Oceanography》2003,59(2):187-200
Wavelet Analysis provides a new orthogonal basis set which is localized in both physical space and Fourier transform space.
Empirical Orthogonal Functions (EOFs), on the other hand, provide a global representation of data sets. Here we investigate
the various ways in which one can combine these basis sets for optimal representation of data. EOFs represent the global large
scale information and wavelet analysis are used to supplement this large scale information with local fine scale information.
Here we begin to explore the application of these two basis sets for outputs from an Ocean General Circulation Model and we
explore various applications, including data assimilation.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
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Max Pfannenstiel 《International Journal of Earth Sciences》1952,40(1):108-109
Ohne ZusammenfassungInhaltsangabe des auf der Klimatagung in Köln am 7. Jan. 1951 gehaltenen Vortrages. 相似文献
328.
Natural Hazards - In order to accommodate the computational burden of high-fidelity storm surge numerical models, surrogate modeling (metamodeling) techniques have gained significant popularity... 相似文献
329.
Liam Courtney‐Davies Sarah E. Gilbert Cristiana L. Ciobanu Simon R. Tapster Marcus W. Richardson Nigel J. Cook Benjamin P. Wade Max R. Verdugo‐Ihl Kathy Ehrig Daniel J. Condon 《Geostandards and Geoanalytical Research》2021,45(1):143-159
In both nature and synthetic experiments, the common iron oxide haematite (α‐Fe2O3) can incorporate significant amounts of U into its crystal structure and retain radiogenic Pb over geological time. Haematite is a ubiquitous component of many ore deposit types and, therefore, represents a valuable hydrothermal mineral geochronometer, allowing direct constraints to be placed on the timing of ore formation and upgrading. However, to date, no suitable natural haematite reference material has been identified. Here, a synthetic haematite U‐Pb reference material (MR‐HFO) is characterised using LA‐ICP‐MS and ID‐TIMS. Centimetre‐scale ‘chips’ of synthesised α‐Fe2O3 were randomly microsampled via laser ablation‐extraction and analysed using ID‐TIMS. Reproducible U/Pb and Pb/Pb measurements were obtained across four separate chips (n = 13). Subsequently, an evaluation of the suitability MR‐HFO in constraining U‐Pb data via LA‐ICP‐MS is presented using a selection of natural samples ranging from Cenozoic to Proterozoic in age. The MR‐HFO normalised U‐Pb ratios are more concordant and ages more accurate versus the same LA‐ICP‐MS spot analyses normalised to zircon reference material, when compared with independently acquired ID‐TIMS data from the same natural haematite grains. Results establish MR‐HFO as a suitable reference material for LA‐ICP‐MS haematite U‐Pb geochronology. 相似文献
330.
Gleb Panteleev Max Yaremchuk Vladimir Luchin Dmitri Nechaev Takashi Kukuchi 《Journal of Oceanography》2012,68(4):485-496
Sea surface height anomalies observed by satellites in 1992–2010 are combined with monthly climatologies of temperature and salinity to estimate circulation in the southern Bering Sea. The estimated surface and deep currents are consistent with independent velocity observations by surface drifters and Argo floats parked at 1,000?m. Analysis reveals 1–3-Sv interannual transport variations of the major currents with typical intra-annual variability of 3–7?Sv. On the seasonal scale, the Alaskan Stream transport is well correlated with the Kamchatka (0.81), Near Strait (0.53) and the Bering Slope (0.37) currents. Lagged correlations reveal a gradual increase of the time the lags between the transports of the Alaskan Stream, the Bering Slope Current and the Kamchatka Current, supporting the concept that the Bering Sea basin is ventilated by the waters carried by the Alaskan Stream south of the Aleutian Arc and by the flow through the Near Strait. Correlations of the Bering Sea currents with the Bering Strait transport are dominated by the seasonal cycle. On the interannual time scale, significant negative correlations are diagnosed between the Near Strait transport and the Bering Slope and Alaskan Stream currents. Substantial correlations are also diagnosed between the eddy kinetic energy and Pacific Decadal Oscillation. 相似文献