Knowledge for Climate/Climate changes Spatial Planning

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Hoe vaak komt extreme neerslag zoals op 28 juli tegenwoordig voor, en is dat anders dan vroeger? \ Weer en klimaat in Nederland [Article]
Oldenborgh, G.J. van \ Lenderink, G. \ 2014
Op 28 juli vielen grote hoeveelheden neerslag in Nederland, op sommige plaatsen ontstond wateroverlast. Hoe vaak komt zoiets voor, en is dat nu vaker dan vroeger? Op basis van een eerste analyse van de meetgegevens vinden we dat de grootste hoeveelhe ...
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De nieuwe KNMI'14-klimaatscenario's voor Nederland \ Meteorologica [Article]
Klein Tank, A.M.G. \ Beersma, J.J. \ Bessembinder, J.J.E. \ Hurk, B.J.J.M. van den \ Lenderink, G. \ Overbeek, B. \ 2014
De opwarming van de aarde die wordt veroorzaakt door de uitstoot van broeikasgassen beinvloedt ook het Nederlandse klimaat, inclusief de zeespiegel. Veel van de huidige klimaattrends zullen in de toekomst doorzetten en maken het noodzakelijk om na te ...
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KNMI’ 14 : klimaatscenario’s voor Nederland : leidraad voor professionals [Monograph]
Klein Tank, A. \ Beersma, J. \ Bessembinder, J. \ Hurk, B. van den \ Lenderink, G. \ 2014
Als de klimaatverandering volgens de scenario’s groot is ten opzichte van de verandering door natuurlijke variaties, dan verschilt het klimaat in de toekomst duidelijk van dat in de afgelopen eeuw. Als de klimaatverandering volgens de scenario’s rela ...
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Extreme precipitation response to climate perturbations in an atmospheric mesoscale model \ Environmental research letters [Scientific article]
Attema, J.J. \ Loriaux, J.M. \ Lenderink, G. \ 2014
Observations of extreme (sub-)hourly precipitation at mid-latitudes show a large dependency on the dew point temperature often close to 14% per degree—2 times the dependency of the specific humidity on dew point temperature which is given by the Clau ...
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De KNMI'14 klimaatscenario's : neerslag en neerslagextremen [Presentation]
Lenderink, G. \ 2014
Presentatie tijdens het Stowa/NHV symposium gevolgen klimaatverandering voor het waterbeheer, 4-5 juni 2014.
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Response of hourly precipitation extremes to climate perturbations: results from a mesoscale model [Presentation]
Lenderink, G. \ 2014
Deltas in Depth Theme 1: Changing weather and impacts, Session DD 1.3: Response of hourly precipitation extremes to climate perturbations: results from a mesoscale model, Dr. Geert Lenderink, KNMI, the Netherlands (2014). Presented at the Internation ...
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Spatial precipitation patterns and trends in The Netherlands during 1951–2009 \ International journal of climatology : a journal of the Royal Meteorological Society [Scientific article]
Daniels, E.E. \ Lenderink, G. \ Hutjes, R.W.A. \ Holtslag, A.A.M. \ 2014
Significant increases in precipitation have been observed in The Netherlands over the last century. At the same time persistent spatial variations are apparent. The objective of this study is to analyse and explain these spatial patterns, focussing o ...
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KNMI’14 : klimaatscenario's voor Nederland [Monograph]
Klein Tank, A. \ Beersma, J. \ Bessembinder, J. \ Hurk, B. van den \ Lenderink, G. \ 2014
Het KNMI presenteert de KNMI'14-klimaatscenario's: vier nieuwe scenario's voor toekomstige klimaatverandering in Nederland. Ieder scenario geeft een samenhangend beeld van veranderingen in twaalf klimaatvariabelen, waaronder temperatuur, neerslag, ze ...
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KNMI ’14 : climate scenarios for the Netherlands : a guide for professionals inclimate adaption [Monograph]
Klein Tank, A. \ Beersma, J. \ Bessembinder, J. \ Hurk, B. van den \ Lenderink, G. \ [2014]
KNMI presents the KNMI’14 climate scenarios: four new scenarios for future climate change in the Netherlands. Each scenario provides a consistent picture of the changes in 12 climate variables, including temperature, precipitation, sea level, and win ...
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SST and circulation trend biases cause an underestimation of European precipitation trends \ Climate dynamics : observational, theoretical and computational research on the climate system [Scientific article]
Haren, R. van \ Oldenborgh, G.J. van \ Lenderink, G. \ Collins, M. \ Hazeleger, W. \ 2013
Clear precipitation trends have been observed in Europe over the past century. In winter, precipitation has increased in north-western Europe. In summer, there has been an increase along many coasts in the same area. Over the second half of the past ...
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The influence of the North Sea on coastal precipitation in the Netherlands in the present-day and future climate \ Climate dynamics : observational, theoretical and computational research on the climate system [Scientific article]
Attema, J.J. \ Lenderink, G. \ 2013
welk thema
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Understanding convective extreme precipitation scaling using observations and an entraining plume model \ Journal of the atmospheric sciences [Scientific article]
Loriaux, J.M. \ Lenderink, G. \ Roode, S.R. de \ Siebesma, A.P. \ 2013
Using a simple entraining plume model, an idealized deep convective environmental temperature profile is perturbed to analyze extreme precipitation scaling from a frequently used relation based on the column condensation rate. The plume model simulat ...
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Evaluation of modeled changes in extreme precipitation in Europe and the Rhine basin \ Environmental research letters [Scientific article]
Haren, R. van \ Oldenborgh, G.J. van \ Lenderink, G. \ Hazeleger, W. \ 2013
In this study, we investigate the change in multi-day precipitation extremes in late winter in Europe using observations and climate models. The objectives of the analysis are to determine whether climate models can accurately reproduce observed tren ...
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The simultaneous occurrence of surge and discharge extremes for the Rhine delta \ Natural hazards and earth system sciences / European Geosciences Union [Scientific article]
Kew, S.F. \ Selten, F.M. \ Lenderink, G. \ Hazeleger, W. \ 2013
The low-lying Netherlands is at risk from multiple threats of sea level rise, storm surges and extreme river discharges. Should these occur simultaneously, a catastrophe will be at hand. Knowledge about the likelihood of simultaneous occurrence or th ...
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KNMI next: welk type aanvullende informatie komt beschikbaar? [Presentation]
Beersma, J. \ Lenderink, G. \ 2012
Presentatie gehouden tijdens workshop KNMInext klimaatscenario's, bij KNMI op 14 februari en 8 maart 2012
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Neerslagverandering in Europa tot nu toe groter dan verwacht \ H twee O : tijdschrift voor watervoorziening en afvalwaterbehandeling [Article]
Haren, R. van \ Oldenborgh, G.J. van \ Lenderink, G. \ Hazeleger, W. \ 2012
In de vorige eeuw onderging de seizoensgemiddelde neerslag boven grote delen van Europa een duidelijke verandering. De gemiddelde neerslag in de winter nam toe in grote delen van Noordwest-Europa, terwijl deze in Zuid-Europa juist afnam. Tijdens de z ...
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High-quality climate projections [Monograph]
Feijt, A.J. \ Lenderink, G. \ Hazeleger, W. \ Schellekens, J. \ Bessembinder, J.J.E. \ Overbeek, B.A. \ Siegmund, P.C. \ [2012]
Midterm assessment report 2012. The fact that climate changes are uncertain poses a challenge when developing adaptation strategies with a long time horizon. Our aim is to mitigate this problem, by studying methods to quantify uncertainty, and develo ...
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Future weather [Monograph]
Lenderink, G. \ Attema, J. \ Kew, S. \ Selten, F. \ Maat, H. ter \ [2012]
The impact of climate change will manifest itself in our future weather. In the project Future Weather we investigated a number of these impact relevant weather conditions in the (present and) future climate. We focussed primarily on changes in preci ...
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Intensiteit van extreme neerslag in een veranderend klimaat \ Weer en klimaat in Nederland [Article]
Lenderink, G. \ Oldenborgh, G.J. van \ Meijgaard, E. van \ Attema, J. \ 2011
Intense buien hebben een grote invloed op de maatschappij en gaan vaak vergezeld met heftige meteorologische verschijnselen zoals onweer, hagel, windstoten, windhozen en tornado’s. Ze kunnen aanleiding geven tot lokale wateroverlast, beperkingen in h ...
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Denk lokaal! : de zin (en onzin) van lokaal modelleren [Presentation]
Lenderink, G. \ 2011
Het gebruik van regionale klimaatmodellen tegenover mondiale modellen. Veel van de onzekerheid in de veranderingen van het regionale klimaat komt door de grotere schaal.
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