The Times of PP, SS, SP and PS     

Michael Shimshoni 《Geophysical Journal International》1966,11(5):477-483

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Changes in magma composition at Arenal volcano,Costa Rica, 1965–1985: Real-time monitoring of open-system differentiation     

Mark K. Reagan  James B. Gill  Eduardo Malavassi  Michael O. Garcia 《Bulletin of Volcanology》1987,49(5):708-708

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Stratification in the lunar regolith — A preliminary view     

Michael B. Duke  J. Stewart Nagle 《Earth, Moon, and Planets》1975,13(1-3):143-158

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AGRICULTURAL DROUGHT ON SOUTH-CENTRAL PACIFIC ISLANDS *     

Thomas W. Giambelluca  Dennis Nullet  Michael A. Nullet 《The Professional geographer》1988,40(4):404-415

A pilot study of spatial patterns of agricultural drought hazard in the south-central Pacific is presented. The durations of crop stress periods are estimated using a water balance approach. A rainfall approach is used to identify dry periods corresponding to different durations. Strong correlation between the results of the two methods indicates that monthly rainfall data are sufficient for estimating the patterns of agricultural drought hazard in the region. The simpler rainfall method is particularly useful for high islands where data required for the water balance approach are not sufficient to characterize the complex climatic patterns. Drought hazard is greatest in the eastern and southwestern parts of the study area. Great spatial variation in drought hazard is observed in a small area on the high islands of Western Samoa, where the range of values found within a few tens of kilometers is about the same as the range found across thousands of kilometers for low islands.  相似文献   

Comet Bowell (1980b): Measurement of the optical thickness of the coma and particle albedo from a stellar occultation     

Stephen M. Larson  Michael F. A&#x;Hearn 《Icarus》1984,58(3):446-450

Comet Bowell (1980b) was observed to pass within 0.25 ± 0.09 arc sec of a star (about 540 km at the comet), where the absorption of starlight by the dust coma was found to be 3% (±1%). The implied optical thickness of 0.03 differs greatly from other determinations and gives a mass of 3 × 10¹³ g for the coma within 1 × 10⁴ km of the nucleus. Coupled with absolute continuum filter photometry, these results indicate a very low particle albedo consistent with fluffy carbonaceous material. This experiment indicates the need to observe nearly central occulations by several observers to measure the optical thickness profile of a comet. The advantages of using a charge-coupled device area photometer for such observations are discussed.  相似文献   

MAN, LAND AND GAME IN SUMBAWA: SOME OBSERVATIONS ON AGRARIAN ECOLOGY AND DEVELOPMENT POLICY IN EASTERN INDONESIA   总被引：2，自引：0，他引：2  

Michael R. Dove  B.A.  Ph.D. 《Singapore journal of tropical geography》1984,5(2):112-124

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Combining pump-and-treat and physical barriers for contaminant plume control     

Bayer P  Finkel M  Teutsch G 《Ground water》2004,42(6-7):856-867

A detailed analysis is presented of the hydraulic efficiency of plume management alternatives that combine a conventional pump-and-treat system with vertical, physical hydraulic barriers such as slurry walls or sheet piles. Various design settings are examined for their potential to reduce the pumping rate needed to obtain a complete capture of a given contaminated area. Using established modeling techniques for flow and transport, those barrier configurations (specified by location, shape, and length) that yield a maximum reduction of the pumping rate are identified assuming homogeneous aquifer conditions. Selected configurations are further analyzed concerning their hydraulic performance under heterogeneous aquifer conditions by means of a stochastic approach (Monte Carlo simulations) with aquifer transmissivity as a random space function. The results show that physical barriers are an appropriate means to decrease expected (mean) pumping rates, as well as the variance of the corresponding pumping rate distribution at any given degree of heterogeneity. The methodology presented can be transferred easily to other aquifer scenarios, provided some basic premises are fulfilled, and may serve as a basis for reducing the pumping rate in existing pump-and-treat systems.  相似文献   

Ground water availability: the challenge ahead in water-scarce regions     

Moran MJ 《Ground water》2004,42(4):480-480

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Trace element residues in tissues of green turtles (Chelonia mydas) from South China waters     

Lam JC  Tanabe S  Chan SK  Yuen EK  Lam MH  Lam PK 《Marine pollution bulletin》2004,48(1-2):174-182

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Geochemistry of coral from Papua New Guinea as a proxy for ENSO ocean–atmosphere interactions in the Pacific Warm Pool     

Linda K. Ayliffe  Michael I. Bird  Michael K. Gagan  Peter J. Isdale  Heather Scott-Gagan  Bruce Parker  David Griffin  Michael Nongkas  Malcolm T. McCulloch 《Continental Shelf Research》2004,24(19):2343-2356

A Porites sp. coral growing offshore from the Sepik and Ramu Rivers in equatorial northern Papua New Guinea has yielded an accurate 20-year history (1977–1996) of sea surface temperature (SST), river discharge, and wind-induced mixing of the upper water column. Depressions in average SSTs of about 0.5–1.0 °C (indicated by coral Sr/Ca) and markedly diminished freshwater runoff to the coastal ocean (indicated by coral δ¹⁸O, δ¹³C and UV fluorescence) are evident during the El Niño – Southern Oscillation (ENSO) events of 1982–1983, 1987 and 1991-1993. The perturbations recorded by the coral are in good agreement with changes in instrumental SST and river discharge/precipitation records, which are known to be diagnostic of the response of the Pacific Warm Pool ocean–atmosphere system to El Niño. Consideration of coastal ocean dynamics indicates that the establishment of northwest monsoon winds promotes mixing of near-surface waters to greater depths in the first quarter of most years, making the coral record sensitive to changes in the Asian–Australian monsoon cycle. Sudden cooling of SSTs by 1°C following westerly wind episodes, as indicated by the coral Sr/Ca, is consistent with greater mixing in the upper water column at these times. Furthermore, the coral UV fluorescence and oxygen isotope data indicate minimal contribution of river runoff to surface ocean waters at the beginning of most years, during the time of maximum discharge. This abrupt shift in flood-plume behaviour appears to reflect the duration and magnitude of northwest monsoon winds, which tend to disperse flood plume waters to a greater extent in the water column when wind-mixing is enhanced. Our results suggest that a multi-proxy geochemical approach to the production of long coral records should provide comprehensive reconstructions of tropical paleoclimate processes operating on interannual timescales.  相似文献