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Statements

Subject Item
n2:RIV%2F25173154%3A_____%2F13%3A%230000266%21RIV13-MSM-25173154
rdf:type
skos:Concept n8:Vysledek
dcterms:description
The present area of European wetlands is only a fraction of their area before the start of large-scale human colonization of Europe. Many European wetlands have been exploited and managed for various purposes. Large wetland areas have been drained and reclaimed mainly for agriculture and establishment of human settlements. These threats to European wetlands persist. The main responses of European wetlands to ongoing climate change will vary according to wetland type and geographical location. Sea level rise will probably be the decisive factor affecting coastal wetlands, especially along the Atlantic coast. In the boreal part of Europe, increased temperatures will probably lead to increased annual evapotranspiration and lower organic matter accumulation in soil. The role of vast boreal wetlands as carbon sinks may thus be suppressed. In central and western Europe, the risk of floods may support the political will for ecosystem-unfriendly flood defence measures, which may threaten the hydrology of existing wetlands. Southern Europe will probably suffer most from water shortage, which may strengthen the competition for water resources between agriculture, industry and settlements on the one hand and nature conservancy, including wetland conservation, on the other. The present area of European wetlands is only a fraction of their area before the start of large-scale human colonization of Europe. Many European wetlands have been exploited and managed for various purposes. Large wetland areas have been drained and reclaimed mainly for agriculture and establishment of human settlements. These threats to European wetlands persist. The main responses of European wetlands to ongoing climate change will vary according to wetland type and geographical location. Sea level rise will probably be the decisive factor affecting coastal wetlands, especially along the Atlantic coast. In the boreal part of Europe, increased temperatures will probably lead to increased annual evapotranspiration and lower organic matter accumulation in soil. The role of vast boreal wetlands as carbon sinks may thus be suppressed. In central and western Europe, the risk of floods may support the political will for ecosystem-unfriendly flood defence measures, which may threaten the hydrology of existing wetlands. Southern Europe will probably suffer most from water shortage, which may strengthen the competition for water resources between agriculture, industry and settlements on the one hand and nature conservancy, including wetland conservation, on the other.
dcterms:title
Actual State of European Wetlands and Their Possible Future in the Context of Global Climate Changes Actual State of European Wetlands and Their Possible Future in the Context of Global Climate Changes
skos:prefLabel
Actual State of European Wetlands and Their Possible Future in the Context of Global Climate Changes Actual State of European Wetlands and Their Possible Future in the Context of Global Climate Changes
skos:notation
RIV/25173154:_____/13:#0000266!RIV13-MSM-25173154
n8:predkladatel
n9:ico%3A25173154
n3:aktivita
n4:P
n3:aktivity
P(2B06023)
n3:cisloPeriodika
1
n3:dodaniDat
n12:2013
n3:domaciTvurceVysledku
n11:2191385
n3:druhVysledku
n5:J
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n15:predkladatel
n3:idSjednocenehoVysledku
59425
n3:idVysledku
RIV/25173154:_____/13:#0000266
n3:jazykVysledku
n14:eng
n3:klicovaSlova
wetlands; carbon sequestration; hydrology; biodiversity; climate stabilization; ecosystem services
n3:klicoveSlovo
n7:wetlands n7:hydrology n7:climate%20stabilization n7:ecosystem%20services n7:biodiversity n7:carbon%20sequestration
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[5922AE96BB53]
n3:nazevZdroje
Aquatic Sciences
n3:obor
n18:EH
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
6
n3:projekt
n17:2B06023
n3:rokUplatneniVysledku
n12:2013
n3:svazekPeriodika
75
n3:tvurceVysledku
Čížková, H. Pithart, D. Laibo, R. Pokorný, Jan Comin, F. A. Květ, J.
s:issn
1015-1621
s:numberOfPages
24