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Freezing level

The freezing level or freezing level height (FLH) represents the altitude in which the temperature in a free atmosphere is at 0 °C , i.e. the freezing point of water. FLH is important for weather in mountainous regions and aviation and over time an indicator of climate variability and climate change.

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Overview

Definition

Uses

History

Measurement

Variations

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Map overview Semantic statistics

Freezing level

Nodes38
Edges37
Triples16
Avg. degree1.95
Density0.052632
Components1

How this topic connects Entity context

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Freezing level

Top relations

related to Definition · 5
Freezing level → Above, Below, FLH, It, The
related to External links · 4
Freezing level → January, NOAA, North American Freezing Level, Tracker
measured by · 2
Freezing level → The, There
related to Uses · 2
Freezing level → The, While
related to Variations · 2
Freezing level → It, The
related to history · 1
Freezing level → The

Important terminology Word statistics

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Important terminology

freezing level height isotherm temperature weather change snow altitude air flh time variations citation needed represents atmosphere point water climate

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
Freezing levelmeasured byThe0.60section
Freezing levelmeasured byThere0.60section
Freezing levelrelated to DefinitionThe0.60section
Freezing levelrelated to DefinitionFLH0.60section
Freezing levelrelated to DefinitionIt0.60section
Freezing levelrelated to DefinitionAbove0.60section
Freezing levelrelated to DefinitionBelow0.60section
Freezing levelrelated to External linksNorth American Freezing Level0.60section
Freezing levelrelated to External linksTracker0.60section
Freezing levelrelated to External linksJanuary0.60section
Freezing levelrelated to External linksNOAA0.60section
Freezing levelrelated to historyThe0.60section

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