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Statements

Subject Item
n2:RIV%2F00216208%3A11320%2F14%3A10272167%21RIV15-MSM-11320___
rdf:type
skos:Concept n20:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.3354/cr01204
dcterms: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.
dcterms:title
Climate classification revisited: from Koppen to Trewartha Climate classification revisited: from Koppen to Trewartha
skos:prefLabel
Climate classification revisited: from Koppen to Trewartha Climate classification revisited: from Koppen to Trewartha
skos:notation
RIV/00216208:11320/14:10272167!RIV15-MSM-11320___
n3:aktivita
n17:Z n17:I
n3:aktivity
I, Z(MSM0021620860)
n3:cisloPeriodika
1
n3:dodaniDat
n13:2015
n3:domaciTvurceVysledku
n14:1688782 n14:7718500 n14:4982231 n14:4582411
n3:druhVysledku
n6:J
n3:duvernostUdaju
n15:S
n3:entitaPredkladatele
n12:predkladatel
n3:idSjednocenehoVysledku
7504
n3:idVysledku
RIV/00216208:11320/14:10272167
n3:jazykVysledku
n7:eng
n3:klicovaSlova
Patton's dryness criteria; CRU TS 3.10.01 dataset; Observed climate change; Climate classification; Koppen; Koppen-Trewartha
n3:klicoveSlovo
n4:CRU%20TS%203.10.01%20dataset n4:Climate%20classification n4:Observed%20climate%20change n4:Patton%27s%20dryness%20criteria n4:Koppen-Trewartha n4:Koppen
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[B03725B76429]
n3:nazevZdroje
Climate Research
n3:obor
n9:DG
n3:pocetDomacichTvurcuVysledku
4
n3:pocetTvurcuVysledku
4
n3:rokUplatneniVysledku
n13:2014
n3:svazekPeriodika
59
n3:tvurceVysledku
Holtanová, Eva Belda, Michal Halenka, Tomáš Kalvová, Jaroslava
n3:wos
000330720600001
n3:zamer
n18:MSM0021620860
s:issn
0936-577X
s:numberOfPages
13
n16:doi
10.3354/cr01204
n10:organizacniJednotka
11320