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  • VHF radar remote sensing of atmospheric parameters over Taiwan during the time period of Typhoon Wayne
  • TSAO, Y. D.
  • JOHNSON, D. L.
  • Palynologic and geomorphic evidence for environmental change during the Pleistocene-Holocene transition at Point Reyes Peninsula, central coastal California
  • The AA. describe the pollen and stratigraphic records of three sites on the Point Reyes. These sites provide a well constrained chronology for the changes in both vegetation and geomorphic processes that occurred during the Pleistocene-Holocene
  • transition. The occurence of debris flows accompanying major aggradation from 12 000 to 10 000 B.P. suggests more intense winter storms during this period.
  • MONTGOMERY, D. R.
  • Clustered streamlined forms in Athabasca Valles, Mars : evidence for sediment deposition during floodwater ponding
  • A unique clustering of layered streamlined forms in Athabasca Valles is hypothesized to reflect a significant hydraulic event. The forms, interpreted as sedimentary, are attributed to extensive sediment deposition during ponding
  • and then streamlining of this sediment behind flow obstacles during ponded water outflow. These streamlined forms are analogous to those found in depositional basins and other loci of ponding in terrestrial catastrophic flood landscapes. Likewise, the streamlined forms
  • BURR, D.
  • Zmiany i zroznicowanie trwania zycia w Polsce w przekroju wojewodzkim. (Changements et différenciation de la durée de vie dans différentes voïvodies en Pologne)
  • tableaux abrégés de la durée de vie pour les années 1973-1975 et 1976-1980. Ces tableaux présentent les paramètres de la durée de vie selon le sexe et une liste des paramètres hypothétiques supposant l'élimination de certains groupes de causes de décès. (D
  • Les changements et la différenciation de la durée de vie, ainsi que le nombre de décès provoqués par différents facteurs, ce qui a une influence sur la durée de vie, constituent l'objet des considérations de l'A., qui s'appuie dans l'analyse sur les
  • Modelling evacuation behavior during the Three Mile Island reactor crisis
  • ZEIGLER, D. J.
  • The structure of the stratosphere in the Southern Hemisphere during late Winter 1973 as observed by satellite
  • HARTMANN D. L.
  • Human populations and cultural adaptations in the Sahara and Nile during prehistoric times in The Sahara and the Nile. Quaternary environments and prehistoric occupation in northern Africa.
  • CLARK, S. D.
  • Faunal and oxygen isotopic evidence for surface water salinity changes during sapropel formation in the eastern Mediterranean
  • WILLIAMS, D. F.
  • European plate movement during the Carboniferous in Evolution of the Earth's crust.
  • TARLING, D. H., (Editeur scientifique)
  • Mass balance and sliding velocity of the Puget lobe of the Cordilleran ice sheet during the last glaciation
  • BOOTH, D. B.
  • Patterns of migration of apprentices into Aberdeen and Inverness during the Eighteenth and early Nineteenth centuries
  • WHYTE, I. D.
  • Sea-level changes in the Netherlands during the Eemian in Special issue in the honour of J. D. De Jong.
  • This paper deals with the determination of relative heights of the sea-level during the Eemian in the Netherlands and adjacent parts of the North Sea region. Eight levels have been established. After the beginning of the Weichselian, the sea-level
  • Sedimentation in the mid-Netherlands river area during the Late Weichselian in Special issue in the honour of J. D. De Jong.
  • Wykorzystanie parametrow fizjograficznych zlewni do okreslania czasu sp ywu wod opadowych Application de paramètres physiographiques d'un bassin-versant à l'estimation de la durée d'écoulement des eaux pluviales
  • Résultats des calculs de la durée d'écoulement des eaux pluviales (durée d'arrivée, durée de concentration) à partir de petits bassins d'origine tardiglaciaire, dans le bassin-versant de la rivière Obra. Les AA. ont fait appel à plusieurs formules
  • WOS, D.
  • Variation of the Köppen C/D climate boundary in the central United States during the 20th century
  • edge of a persistent snow cover during winter. The most anomalous feature for the decadal maps is the distinct southerly location of the C/D boundary for the recent decade of the 1970s. This study does not provide evidence of a trend toward wintertime
  • The spatial and temporal variation of the C/D Köppen climate boundary in the central United States is examined for the period 1900 to 1999. The C/D climate boundary is determined by differences in winter conditions. It represents the equatorward
  • warming and a northerly migration of the C/D climate boundary within the central United States.
  • Comparison of SAGE II ozone measurements and ozone soundings at Uccle (Belgium) during the period February 1985 to January 1986
  • is in general quite good, especially for profiles nearly coincident in time and space, and during periods of little dynamic activity over the area considered.
  • DE MUER, D.
  • Palaeogeographic evolution and seismotectonic implications of the broader area of Eurotas River (Greece) during the Quaternary
  • of the area during the Quaternary, and finally to draw some conclusions regarding the seismic hazards of this area.
  • PAPANASTASSIOU, D.
  • Pathways of dust input to the Chinese Loess Plateau during the last glacial and interglacial periods
  • decrease downwind from the dust source, the spatial distribution of dust sedimentation rates shows that northwest and west winds were the 2 most important agents for transport of dust to the Loess Plateau during the last glacial cycle.
  • SUN, D.
  • Thresholds and the spatial variability of flood power during extreme floods
  • , and will directly and indirectly control flood power within the drainage network through its control on the rates of change of several hydraulic variables during discharge increases.
  • PHILLIPS, J. D., (Editeur scientifique)
  • Alpine evidence for atmospheric circulation patterns in Europe during the Last Glacial Maximum
  • the atmospheric circulation and associated precipitation patterns responsible for the ice buildup in the Alps during the last glaciation and 2) an explanation for the nonsynchronous maximum glacial extents in the Alps, the Pyrénées, and the surrounding low
  • FLORINETH, D.