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Will dry events occur more often in Hungary in the future?

by Philip Lorenz, Daniela Jacob , 2007
"... Dry years and dry summers in Hungary have been analyzed using the regional climate model REMO for the time periods 1961–2000 and 2001–2100. Dry periods were determined and classified by intensity, considering modeled and observed precipitation and temperature data. The intensity of dry events was de ..."
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Dry years and dry summers in Hungary have been analyzed using the regional climate model REMO for the time periods 1961–2000 and 2001–2100. Dry periods were determined and classified by intensity, considering modeled and observed precipitation and temperature data. The intensity of dry events

Market liquidity and funding liquidity.

by Markus K Brunnermeier , Heje Lasse , Pedersen , Franklin Allen , Yakov Amihud , David Blair , Bernard Dumas , Denis Gromb , Charles Johns , Christian Julliard , John Kambhu , Filippos Markus Konz , Pa-Pakonstantinou , Ketan Patel , Guillaume Plantin , Jeremy Stein , Dimitri Vayanos , Jiang Wang , Pierre-Olivier Weill , 2009
"... Abstract We provide a model that links a assets' market liquidity -i.e., the ease of trading it -and traders' funding liquidity -i.e., their availability of funds. Traders provide market liquidity and their ability to do so depends on their funding. Conversely, traders' funding, i.e. ..."
Abstract - Cited by 440 (13 self) - Add to MetaCart
that market liquidity (i) is fragile, i.e. can suddenly dry up, (ii) has commonality across securities, (iii) is related to volatility, (iv) experiences "flight to liquidity" events, and (v) comoves with the market.

Wet and Dry Analysis for the Cagayan Valley, the Philippines

by Huynh Ngoc Tan, Carlos C, Huynh N Goc Phien, Carlos C. T An
"... In this first step toward a regional analysis of wet and dry events, the theory of runs is coupled with a multi-site data generation technique in order to serve two purposes. The first one is to define the parameters of the wet and dry events in terms of the runs-charac-teristics such as the run-len ..."
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In this first step toward a regional analysis of wet and dry events, the theory of runs is coupled with a multi-site data generation technique in order to serve two purposes. The first one is to define the parameters of the wet and dry events in terms of the runs-charac-teristics such as the run

2009: Intraseasonal and interannual variability of extreme dry and wet events over southeastern South America and the subtropical Atlantic during austral summer

by Michel N. Muza, Leila M. V. Carvalho, Charles Jones, Brant Liebmann - Journal of Climate
"... Intraseasonal and interannual variability of extremewet and dry anomalies over southeasternBrazil and the western subtropical South Atlantic Ocean are investigated. Precipitation data are obtained from the Global Precipitation Climatology Project (GPCP) in pentads during 23 austral summers (December ..."
Abstract - Cited by 3 (0 self) - Add to MetaCart
(December–February 1979/ 80–2001/02). Extreme wet (dry) events are defined according to 75th (25th) percentiles of precipitation anomaly distributions observed in two time scales: intraseasonal and interannual. The agreement between the 25th and 75th percentiles of theGPCP precipitation and gridded

Drying and hydrophobic collapse of paraffin plates

by Xuhui Huang, Ruhong Zhou, Bruce J. Berne - J. Phys. Chem. B
"... We perform molecular dynamics simulations of the hydrophobic collapse of two paraffin plates to examine how the collapse is mediated by realistic paraffin-water attractive van der Waals forces. We explore several aspects of the drying transition between the plates, including the critical separation ..."
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for drying and the critical size of the vapor bubble required for the nucleation of the drying event. We also investigate the kinetics of hydrophobic collapse and find that the hydrophobic collapse occurs in about 100 ps. We compare these results with the simulations with the plate-water van der Waals

STATISTICAL ANALYSIS AND TRENDS OF DRY DAYS IN

by Syed Mustakim, Ali Shah, G. M. Jahid Hasan , 2013
"... Abstract:  The rainfall distribution in Bangladesh is not uniform and reflecting topography. Hilly Sylhet region receives substantial rainfall every year compare to other regions of Bangladesh. Though Sylhet region is less vulnerable to drought but weather pattern is not constant and changing day by ..."
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to investigate extreme dry events, time history of monthly dry days data were transformed into frequency domain using the Fast Fourier Transform (FFT). Variability of dry days in time scale was also checked from filtered signals which is very useful for drought analysis, agricultural development and disaster

2005), Representation of dry tropical layers and their origins in ERA‐40 data

by Piero Cau, John Methven, Brian Hoskins
"... [1] The focus of this paper is the occurrence of dry intrusions in the tropical atmosphere and their origin. Dry layers are observed to have a wide range of thicknesses, so as guidance on the scales of interest the radiative impact of dry intrusions is investigated. Typically such intrusions would c ..."
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and December 1992 at Kapingamarangi, in the tropical West Pacific.Avariety of behaviors is found,withmany dry events clearly associatedwith air masses descending from the extratropics. Four particular dry events are discussed.

Determination of Best-fit Distribution and Rainfall Events in Damansara and Kelantan, Malaysia 1

by Ho Ming Kang, Fadhilah Yusof
"... Abstract This paper presents a study to determine the best-fit distribution to represent the rainfall process in Damansara and Kelantan, Malaysia. Three probability density functions, namely Wakeby distribution, Generalized Extreme Value function (GEV) and two-parameter Weibull distributions are sel ..."
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and Kelantan is used to identify the occurrence of wet and dry events in the rainfall data. The impact of different distributions used in the determination of rainfall events is evaluated by making comparison between the actual and the reconstructed rainfall data. The results indicate that the Wakeby

Scale Invariant Events and Dry Spells for Medium Resolution Local Rain Data

by Anna Deluca , 2014
"... Abstract. We analyze distributions of rain-event sizes, rain-event durations, and dry-spell durations for data obtained from a network of 20 rain gauges scattered in a region of the NW Mediterranean coast. While power-law distribu-tions model the dry-spell durations with a common expo-nent 1.50±0.05 ..."
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Abstract. We analyze distributions of rain-event sizes, rain-event durations, and dry-spell durations for data obtained from a network of 20 rain gauges scattered in a region of the NW Mediterranean coast. While power-law distribu-tions model the dry-spell durations with a common expo-nent 1

Modelling of Dynamic and Quasistatic Events with Special Focus on Wood-Drying Distortions

by Mats Ekevad, Mats Ekevad , 2006
"... Mats Ekevad Modelling of dynamic and quasistatic events with special focus on wood-drying distortions Cover: colourful picture made on the computer by Mats Ekevad, “Flying board” Mats Ekevad Modelling of dynamic and quasistatic events with special focus on wood-drying distortions This thesis deals m ..."
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Mats Ekevad Modelling of dynamic and quasistatic events with special focus on wood-drying distortions Cover: colourful picture made on the computer by Mats Ekevad, “Flying board” Mats Ekevad Modelling of dynamic and quasistatic events with special focus on wood-drying distortions This thesis deals
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