zero degree tooth - Definition. Was ist zero degree tooth
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Was (wer) ist zero degree tooth - definition

Zero degree isotherm; ISO 0 degrees
  • Dual-polarization radar image of an easily identifiable freezing layer, denoted by the yellow ring around the radar.

Zero Degree         
NOVEL BY CHARU NIVEDITA
Zero degree
Zero Degree is a postmodern, transgressive, lipogrammatic novel written in 1998 by Tamil author Charu Nivedita, later translated into Malayalam and English.
Degree (graph theory)         
  • Two non-isomorphic graphs with the same degree sequence (3, 2, 2, 2, 2, 1, 1, 1).
  • An undirected graph with leaf nodes 4, 5, 6, 7, 10, 11, and 12
NUMBER OF EDGES INCIDENT TO A GIVEN VERTEX IN A NODE-LINK GRAPH
In degree; Valency (mathematics); In degree (graph theory); Out degree (graph theory); Valency (graph theory); Out degree; Vertex degree; Degree sequence; Graphic sequence; Graphical sequence; Degree of a graph; Even degree; Degree of a vertex
In graph theory, the degree (or valency) of a vertex of a graph is the number of edges that are incident to the vertex; in a multigraph, a loop contributes 2 to a vertex's degree, for the two ends of the edge.Diestel, pp.
Zero (art)         
  • Günther Uecker, photo by Lothar Wolleh
  • Otto Piene, photo by Lothar Wolleh
  • Günther Uecker, Gropiusbau, Berlin
  • ZERO, Guggenheim, New York
GROUP OF ARTISTS
ZERO foundation
Zero (usually styled as ZERO) was an artist group founded in the late 1950s in Düsseldorf by Heinz Mack and Otto Piene. Piene described it as "a zone of silence and of pure possibilities for a new beginning".

Wikipedia

Freezing level

The freezing level, or 0 °C (zero-degree) isotherm, represents the altitude in which the temperature is at 0 °C (the freezing point of water) in a free atmosphere (i.e. allowing reflection of the sun by snow, icing conditions, etc.). Any given measure is valid for only a short period of time, often less than a day as variations in wind, sunlight, air masses and other factors may change the level.

Above the freezing altitude, the temperature of the air is below freezing. Below it, the temperature is above freezing. The profile of this frontier, and its variations, are studied in meteorology, and are used for a variety of forecasts and predictions, especially in cold weather. Whilst not given on general weather forecasts, it is used on bulletins giving forecasts for mountainous areas.