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Description
  • The analysis of climate patterns can be performed separately for each climatic variable or the data can be aggregated, for example, by using a climate classification. These classifications usually correspond to vegetation distribution, in the sense that each climate type is dominated by one vegetation zone or eco-region. Thus, climatic classifications also represent a convenient tool for the validation of climate models and for the analysis of simulated future climate changes. Basic concepts are presented by applying climate classification to the global Climate Research Unit (CRU) TS 3.1 global dataset. We focus on definitions of climate types according to the Koppen- Trewartha climate classification (KTC) with special attention given to the distinction between wet and dry climates. The distribution of KTC types is compared with the original Koppen classification (KCC) for the period 1961- 1990. In addition, we provide an analysis of the time development of the distribution of KTC types throughout the 20th century. There are observable changes identified in some subtypes, especially semi-arid, savanna and tundra.
  • The analysis of climate patterns can be performed separately for each climatic variable or the data can be aggregated, for example, by using a climate classification. These classifications usually correspond to vegetation distribution, in the sense that each climate type is dominated by one vegetation zone or eco-region. Thus, climatic classifications also represent a convenient tool for the validation of climate models and for the analysis of simulated future climate changes. Basic concepts are presented by applying climate classification to the global Climate Research Unit (CRU) TS 3.1 global dataset. We focus on definitions of climate types according to the Koppen- Trewartha climate classification (KTC) with special attention given to the distinction between wet and dry climates. The distribution of KTC types is compared with the original Koppen classification (KCC) for the period 1961- 1990. In addition, we provide an analysis of the time development of the distribution of KTC types throughout the 20th century. There are observable changes identified in some subtypes, especially semi-arid, savanna and tundra. (en)
Title
  • Climate classification revisited: from Koppen to Trewartha
  • Climate classification revisited: from Koppen to Trewartha (en)
skos:prefLabel
  • Climate classification revisited: from Koppen to Trewartha
  • Climate classification revisited: from Koppen to Trewartha (en)
skos:notation
  • RIV/00216208:11320/14:10272167!RIV15-MSM-11320___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, Z(MSM0021620860)
http://linked.open...iv/cisloPeriodika
  • 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 7504
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11320/14:10272167
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Patton's dryness criteria; CRU TS 3.10.01 dataset; Observed climate change; Climate classification; Koppen; Koppen-Trewartha (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV
  • [B03725B76429]
http://linked.open...i/riv/nazevZdroje
  • Climate Research
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 59
http://linked.open...iv/tvurceVysledku
  • Belda, Michal
  • Halenka, Tomáš
  • Holtanová, Eva
  • Kalvová, Jaroslava
http://linked.open...ain/vavai/riv/wos
  • 000330720600001
http://linked.open...n/vavai/riv/zamer
issn
  • 0936-577X
number of pages
http://bibframe.org/vocab/doi
  • 10.3354/cr01204
http://localhost/t...ganizacniJednotka
  • 11320
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