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Wave climatology of the southeastern Mediterranean
The wave climate of the southeastern Mediterranean is defined here for the first time by integrating 57 326 visual observations and gauge measurements including wave height, period and direction, from five different sources during the years 1948

A classification of sand wave in alluvial stream.
The concept of sand waves in stream beds is discussed and the principles for their classification examined. The classification divides waves into two grades| the first covers two subdivisions and the second covers six. Each is defined and described

Cold waves and winter monsoon in East Asia : with special reference to south China
Definition of cold waves from the statistical and synoptic climatological standpoints| cold airmass movement stream lines and wind component for the main three types of cold waves in south China| cold waves by the Geostationary Meteorological
Satellite Himawari images in winter 1986/87 and typical cold waves in relation to winter monsoon situations such as the cases in January and February 1963.

Beobachtungen von atmosphärischen Schwerewellen mit einem Schwerewellen-Messnets. (Observations of atmospheric gravity waves with a gravity waves measuring network)
A stationary measuring network for atmospheric gravity waves in the lower atmosphere is described. It is located at Juliusruh (Rügen/GDR) and consists of three sensor stations with data telemetry and primery data processing by microprocessor

Ocean wave parameter measurement using a dual-radar system. A simulation study

Sediment waves and other evidence of paleobottom currents at two locations in the deep Arctic Ocean

Seismic waves and sources.

Stratospheric long waves: comparison of thermal structure in the Northern and Southern Hemispheres

Beach cusps formed by intersecting waves

High frequency radar observations of horizontal plasma waves in the equatorial ionosphere

In this paper the double Fourier series technique is used to model two doline and two cockpit karst landscapes in northern Jamaica. This is done : 1) to see how well these karst terrains can be approximated by a series of wave surfaces, 2) to assess
the degree of organization within these complex landscapes in terms of the forms of the principal waves needed to model them, and 3) to assess the potential of the method to differentiate between karst styles by determining if the properties of the waves used

Evidence for transport of bedload in waves: analysis of fluvial sediment samples in a small upland stream channel
In extremely arid, rocky, high relief watersheds, coarse fluvial sediment, if initially entrained, tends to group itself in well defined waves which move discretly downstream. Above a certain threshold determined by stream power this movement

Observations of mountain-wave event over the Pyrenees
The airflow over the Pyrenees on March 23, 1982 was an important mountain wave event. As observed during foehn (Alps) or during chinook (Rocky Mountains), the impact of the barrier leads to a destabilization of the leeward atmosphere. The event

Sediment accumulation in low sedimentation, wave-dominated, glaciated inlets in Sedimentology of fjords.
Many fjords situated in lowland areas of resistant bedrock are characterized by a comparatively low fluvial sediment flux and are often dominated by wave processes. Several such fjords in Eastern Canada are used as examples to develop a generalized
sediment distribution model. Storm waves resuspend fine-grained sediment in water depths of tens of metres and produce near bottom turbid water zones within basins. Fine sands and silt settle out rapidly, leading to the deposition of graded beds

Studies of prograded sectors of sandy coastline in Victoria have shown that some are initiated upon wave-built beach berms colonised by dune vegetation that begins to trap wind blown sand| others develop where backshore terraces built under dune
vegetation spreading from pre-existing dunes are trimmed back by storm wave erosion, forming a dune cliff capped by spillover sand which becomes a foredune as further aeolian accretion proceeds. A berm is defined as an impersistant wave-built ridge or terrace
on the beach face| a beach ridge is a more persistent wave-built ridge formed at or above high spring tide on a prograding sandy coast| a foredune is a ridge of aeolian sand running parallel to the coastline. (L'A.).

Effect of fire and associate heating wave on the physicochemical parameters related to the soil potential erodability

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