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Dungeness foreland: its shingle ridges and what lies under them
  • Dungeness foreland: its shingle ridges and what lies under them
Holocene transgressive-regressive sequence in Yangtze delta area.
  • LI CONGXIAN
  • LI PING
Morphology of cobble streams is small watersheds
  • LI Ruh-Ming
Raspolagajutsja li lednikovye cirki gornyh stran na opredelennyh vysotnyh urovnjah, i esli da, to cem opredeljajutsja eti urovni? Les cirques glaciaires des régions montagneuses sont-ils disposés à des altitudes déterminées, et si oui, par quoi ces niveaux sont-ils déterminés?
  • Raspolagajutsja li lednikovye cirki gornyh stran na opredelennyh vysotnyh urovnjah, i esli da, to cem opredeljajutsja eti urovni? Les cirques glaciaires des régions montagneuses sont-ils disposés à des altitudes déterminées, et si oui, par quoi ces
Mozno li sudit'o transpiracii lesa po velicine ego produktivnosti? Peut-on juger de la transpiration d'une forêt d'après la valeur de sa productivité?
  • Mozno li sudit'o transpiracii lesa po velicine ego produktivnosti? Peut-on juger de la transpiration d'une forêt d'après la valeur de sa productivité?
The granulometrical characteristics of a slowly-moving dust cloud
  • The granulometrical border between eolian transport in saltation and eolian transport in suspension lies, according to the results of the experiment, at a diameter of about 63 m.
Control of seawater composition
  • The chemistry of the lanthanides is compared with that of alkali and alkaline earth metals with a similar electronegativity (the lithium group Li, Mg, Ca, Sr) to confirm that solid state chemistry plays a major part in controlling the composition
Climatic problems of Quaternary glaciation in the Eastern China mountains.
  • LI, Ji-jun
Prospects for Quaternary pollen research in China.
  • LI, Wen-yi
Thermal seasonality of the high mountain belts of the Pyrenees in Special issue on the Spanish Pyrenees.
  • Presentation of altitudinal gradients of thermal variables and seasonal means as regression equations which allows extrapolation of such variables to a range of altitudes. The lowest critical isotherm, O C for the period December-March, lies
A preliminary study on the climatic and environmental changes at the turn from Pleistocene to Holocene in East Asia in Tibet and High-Asia-Results of the Sino-German Point expeditions.
  • LI TIANCHI
The spring in the forest terrain at Svartberget, Northern Sweden
  • this relationship on three points. Two of the points lie on a glacial till slope, one in an old spruce forest and the other in a clear felled area. The third point lies on a clear felled area on level sediment. This study mainly deals with the period when the soils
Gestaltung wassergefüllter Solle in der Agrarlandschaft. (Formation of water-filled kettle holes in the rural landscape)
  • On the basis of field investigations at water-filled hollow moulds (kettle holes) in Ostbrandenburg the density of this landscape element, the function and the efficiency in the rural landscape were analysed. The focus of this investigation lies
Wave spectrum analysis of height fields at 100 MB over the northern hemisphere.
  • LI, Xi-jun
Classification et lignes de fort gradient pour l'interprétation d'une image Thematic Mapper
  • LI, W.
Utilization of the computerized mapping in ecological research
  • LI WEN-HUA
A preliminary research on flood risk forecasting information system in Geographic information system development in China.
  • LI, H.
Late Quaternary Monsoon patterns on the Loess Plateau of China
  • LI JIJUN
Plan form and profile form of hillslopes
  • be described as wholly concave in plan where P is less than 40, wholly convex in plan where P is greater than +40 and convexo-concave in plan where P lies between 40 and +40. One mesure of P taken at the profile sampling line is found to give a better estimate
Climatic relationships of permafrost zones in areas of low winter snow-cover
  • between discontinuous and sporadic permafrost lies just on the cold side of 0C MAAT. The sporadic permafrost zone includes the zone of ice caves and the regions with patches of ice beneath ponds and peatbogs, out to 5C MAAT at a thawing index of 4000