2011
DOI: 10.1007/978-90-481-9834-4
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Forest Management and the Water Cycle

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Cited by 26 publications
(7 citation statements)
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“…This is a very important parameter (it is much more often applied, e.g., in agriculture) that often indicates the probability of tree survival under unfavorable environmental conditions. This can be demonstrated by comparing several Norway spruce stands with different soil water regimes and stand densities (Cermák & Nadezhdina 2011a, 2011b. Similar, but still modified information represents, e.g., cambium area index related ratio, CAI/( RAIabs/LAIsun), etc.…”
Section: Examples Of the Application Of Active Absorptive Root Systemmentioning
confidence: 90%
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“…This is a very important parameter (it is much more often applied, e.g., in agriculture) that often indicates the probability of tree survival under unfavorable environmental conditions. This can be demonstrated by comparing several Norway spruce stands with different soil water regimes and stand densities (Cermák & Nadezhdina 2011a, 2011b. Similar, but still modified information represents, e.g., cambium area index related ratio, CAI/( RAIabs/LAIsun), etc.…”
Section: Examples Of the Application Of Active Absorptive Root Systemmentioning
confidence: 90%
“…Additional methods are being developed and are also used for practical applications in the open field. We are not presenting a comprehensive excellent review as published recently (see Huttunen et al 2001, Bredemeier et al 2011, Meinzer et al 2011, Mancuso 2012). Instead, we are focusing only on providing a brief description of methods that we have actually tested under open forest conditions (mostly outside permanent research plots) and with which we have obtained good results.…”
Section: Introductionmentioning
confidence: 97%
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“…An additional way of avoiding this dilemma of uncertainty is to reduce the time scale of management planning (Lode, Langensiepen, Roosaare, Schüler, & Koivusalo, 2011). In this sense, decisions should not be taken too early and several options should be considered, such as dealing with increasingly frequent droughts on one hand and increased runoff generation on the other hand.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…Even in the regions that may not see significant changes in precipitation, warmer temperatures can increase water demands and evaporation, putting greater stress on water supplies (IPCC, 2014;Rowell & Jones, 2006;Schär et al, 2004;Škvarenina, Krížová, & Tomlain, 2004). Higher air temperatures are assumed to cause more pronounced drought impact on water loss from plants due to increased water vapour deficit, resulting in increased potential transpiration (Centritto, Tognetti, Leitgeb, Střelcová, & Cohen, 2011).…”
mentioning
confidence: 99%