Population bound effects on bosonic correlations in non-inertial frames

We analyse the effect of bounding the occupation number of bosonic field modes on the correlations among all the different spatial-temporal regions in a setting in which we have a space-time with a horizon along with an inertial observer. We show that the entanglement between A (inertial observer) and R (uniformly accelerated observer) depends on the bound N, contrary to the fermionic case. Whether or not decoherence increases with N depends on the value of the acceleration a. Concerning the bipartition A-antiR (Alice with an observer in Rindler's region IV), we show that no entanglement is created whatever the value of N and a. Furthermore, AR entanglement is very quickly lost for finite N and for infinite N. We will study in detail the mutual information conservation law found for bosons and fermions. By means of the boundary effects associated to N finiteness, we will show that for bosons this law stems from classical correlations while for fermions it has a quantum origin. Finally, we will present the strong N dependence of the entanglement in R-antiR bipartition and compare the fermionic cases with their finite N bosonic analogs. We will also show the anti-intuitive dependence of this entanglement on statistics since more entanglement is created for bosons than for their fermion counterparts.Comment: revtex 4, 12 pages, 10 figures. Added Journal ref

Unveiling quantum entanglement degradation near a Schwarzschild black hole

We analyze the entanglement degradation provoked by the Hawking effect in a bipartite system Alice-Rob when Rob is in the proximities of a Schwarzschild black hole while Alice is free falling into it. We will obtain the limit in which the tools imported from the Unruh entanglement degradation phenomenon can be used properly, keeping control on the approximation. As a result, we will be able to determine the degree of entanglement as a function of the distance of Rob to the event horizon, the mass of the black hole, and the frequency of Rob's entangled modes. By means of this analysis we will show that all the interesting phenomena occur in the vicinity of the event horizon and that the presence of event horizons do not effectively degrade the entanglement when Rob is far off the black hole. The universality of the phenomenon is presented: There are not fundamental differences for different masses when working in the natural unit system adapted to each black hole. We also discuss some aspects of the localization of Alice and Rob states. All this study is done without using the single mode approximation.Comment: 16 pages, 10 figures, revtex4. Added Journal referenc

Climate of an oceanic island in the Eastern Pacific: Isla del Coco, Costa Rica, Central America

Studies of atmosphere-ocean interaction in the Pacific of Costa Rican are scarce. To identify oceanographic systems that may be influencing climate near Cocos Island (Eastern Tropical Pacific Seascape) we conducted six scientific expeditions between 2007 and 2012. Two automated weather stations were set near Chatham and Wafer bays during the expeditions. Data included records from National Meteorological Institute, Global Precipitation Climatology Project (GPCP) and Extended Reconstructed Sea Surface Temperature (ERSST). The climate is typical of the Eastern Tropical Pacific. Its seasonality is driven by precipitation variability associated with meridional migration of the Intertropical Convergence Zone. The seasonal cycle has two peaks, in May and July, a relative minimum between them in June, and the absolute minimum in February. Most of the precipitation is recorded from April to November. Most rain events have short duration and low intensity. An SST trend was observed from January 1854 to December 2013, coherent with regional warming temperature observations. From 1998 to 2013 there were changes in distributions of almost all meteorological parameters. The combination of these factors resulted in higher evapotranspiration values through the daily cycle, especially during the night time. Precipitation (P) positive anomalies tended to be associated with positive air surface temperature (AST) and SST anomalies and negative global radiation (GR) anomalies. Negative P anomalies tended to be associated with negative AST, SST and positive GR anomalies. Relative humidity (RH) negative anomalies tend to be associated with positive wind speed (WS) anomalies, and the WS effect is opposite for positive RH anomalies. During the cold Niño 3 condition of October 2007, negative P, AST, SST and RH anomalies were observed in concordance with positive WS and GR anomalies, in agreement with the conceptual model of climate system response at Isla del Coco to cold ENSO conditions.Estudios de la interacción atmósfera-océano en el Pacífico de Costa Rica son escasos. Para identificar los sistemas oceanográficos que pueden estar influyendo el clima cerca de la Isla del Coco (Corredor de Protección Marina del Pacífico Tropical del Este), realizamos seis expediciones científicas entre 2007 y 2012. Dos estaciones meteorológicas automáticas fueron instaladas cerca de las bahías de Chatham y Wafer durante las expediciones. Entre los datos se incluyeron registros del Instituto Meteorológico Nacional, el Proyecto de Climatología Global de Precipitación (GPCP por sus siglas en inglés) y la Reconstrucción Extendida de Temperatura Superficial del Mar (ERSST por sus siglas en inglés). El clima es típico del Pacífico Tropical del Este. Su estacionalidad está impulsada por la variabilidad en la precipitación asociada con la migración meridional de la Zona de Convergencia Intertropical. El ciclo anual de precipitación tiene dos picos en mayo y julio, un mínimo relativo entre ellos en junio, y un mínimo absoluto en febrero. La mayoría de la precipitación se registra de abril a noviembre. La mayoría de los eventos tienen corta duración y baja intensidad. Una tendencia en temperatura superficial del mar (TSM) fue observada de enero 1854 a diciembre 2013, coherente con las observaciones de calentamiento en la región. De 1998 a 2013 hubo cambios en las distribuciones de casi todos los parámetros meteorológicos. La combinación de estos factores resultó en tasas más altas de evapotranspiración a través del ciclo diario, especialmente durante la noche. Anomalías positivas de precipitación (P) tienden a ser asociados con anomalías positivas de temperatura superficial del aire (TSA) y de TSM, y con anomalías negativas de radiación global (RG). Anomalías negativas de P tienden a ser asociadas con anomalías negativas de TSA, TSM y anomalías positivas de RG. Anomalías negativas de humedad relativa (HR) tienden a ser asociadas con anomalías positivas de velocidad del viento (VV), y el efecto de la VV es opuesto para anomalías positivas de HR. Durante la condición fría de Niño 3 de octubre del 2007, anomalías negativas de P, TSA, TSM y HR fueron observadas en concordancia con anomalías positivas de VV y RG, de acuerdo con el modelo conceptual de la respuesta del sistema climático en la Isla del Coco ante condiciones frías de ENOS

Tropical Cyclones Losses by Economic Sector in Costa Rica, Central America

Tropical cyclones normally affect Central America and Costa Rica. Population growth and inefficient land use planning increases the exposure to natural hazards related to tropical cyclones such as landslides and floods. The Ministry of National Planning and Economic Policy of Costa Rica gathered all the economic impacts by municipality in every economic sector since Hurricane Joan in 1988. Our results indicate that road infrastructure, agriculture, sewerage, and housing were the most affected economic sectors in the last three decades in the country. Normally, the Pacific basin municipalities are the most affected units due to the indirect impact of tropical cyclones in Costa Rica. These results unravel the most affected municipalities and economic sectors by tropical cyclones in the country and is a useful approach that can be applied to other countries and regions affected by these phenomena throughout the tropics.Universidad de Costa Rica/[805-B9-454]/UCR/Costa RicaUniversidad de Costa Rica/[805-C0-610]/UCR/Costa RicaUniversidad de Costa Rica/[805-A4-906]/UCR/Costa RicaUniversidad de Costa Rica/[805-B0-810]/UCR/Costa RicaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)UCR::Vicerrectoría de Docencia::Ciencias Sociales::Facultad de Ciencias Sociales::Escuela de Geografí

High-level quinolone resistance is associated with the overexpression of smeVWX in Stenotrophomonas maltophilia clinical isolates

AbstractStenotrophomonas maltophilia is the only known bacterium in which quinolone-resistant isolates do not present mutations in the genes encoding bacterial topoisomerases. The expression of the intrinsic quinolone resistance elements smeDEF, smeVWX and Smqnr was analysed in 31 clinical S. maltophilia isolates presenting a minimum inhibitory concentration (MIC) range to ciprofloxacin between 0.5 and > 32 μg/mL; 11 (35.5%) overexpressed smeDEF, 2 (6.5%) presenting the highest quinolone MICs overexpressed smeVWX and 1 (3.2%) overexpressed Smqnr. Both strains overexpressing smeVWX presented changes at the Gly266 position of SmeRv, the repressor of smeVWX. Changes at the same position were previously observed in in vitro selected S. maltophilia quinolone-resistant mutants, indicating this amino acid is highly relevant for the activity of SmeRv in repressing smeVWX expression. For the first time SmeVWX overexpression is associated with quinolone resistance of S. maltophilia clinical isolates

Use of PCR to detect infection of differentially susceptible maize cultivars using Ustilago maydis strains of variable virulence

Ustilago maydis was specifically detected in infected maize plants by means of the polymerase chain reaction (PCR) using oligonucleotides corresponding to a specific region downstream of the homeodomain of the bE genes of the pathogen. The reaction gave rise to amplification of a ca. 500-bp product when tested with U. maydis DNA, but no amplification was detected with DNA from fungi not related to U. maydis. Using these primers, U. maydis was detected in infected maize plants from differentially susceptible cultivars as early as 4 days after inoculation with strains of variable degrees of virulence. Detection of U. maydis at early stages of infection, or in asymptomatic infected plants should assist in studies on plant–pathogen interactions

The entangling side of the Unruh-Hawking effect

We show that the Unruh effect can create net quantum entanglement between inertial and accelerated observers depending on the choice of the inertial state. This striking result banishes the extended belief that the Unruh effect can only destroy entanglement and furthermore provides a new and unexpected source for finding experimental evidence of the Unruh and Hawking effects.Comment: 4 pages, 4 figures. Added Journal referenc

Quantum correlations through event horizons: Fermionic versus bosonic entanglement

We disclose the behaviour of quantum and classical correlations among all the different spatial-temporal regions of a space-time with an event horizon, comparing fermionic with bosonic fields. We show the emergence of conservation laws for entanglement and classical correlations, pointing out the crucial role that statistics plays in the information exchange (and more specifically, the entanglement tradeoff) across horizons. The results obtained here could shed new light on the problem of information behaviour in non-inertial frames and in the presence of horizons, giving a better insight about the black hole information paradox.Comment: 15 pages, 8 figures, revtex 4, title changed to match journal publication and Journal reference adde

Visualization of 40 Years of Tropical Cyclone Positions and Their Rainfall

Correos de investigadores: [email protected] || [email protected] || [email protected] || [email protected] article focuses on a visualization of tropical cyclone track data occurring over a 40- year period (1970–2010) and their relationship with (extremely) heavy rainfall reported by 88 Central American weather stations. The purpose of the visualization is to associate the paths of tropical cyclones in oceanic areas with heavy rainfall inland. Thus, the potential for producing a set of rainfall patterns might somehow help in predicting where different impacts like flooding might occur when tropical cyclones develop in specific oceanic regions. The visualization will serve as a key tool for CIGEFI scientists to apply in their work to determine critical positions of the tropical cyclones associated with extremely heavy rainfall events at daily timescales.Universidad de Costa Rica/[805-B9-454]/UCR/Costa RicaUniversidad de Costa Rica/[805-C0-610]/UCR/Costa RicaUniversidad de Costa Rica/[EC-497]/UCR/Costa RicaUniversidad de Costa Rica/[805-A4-906]/UCR/Costa RicaUniversidad de Costa Rica/[805-C0-074]/UCR/Costa RicaUniversidad de Costa Rica/[805-A1-715]/UCR/Costa RicaUniversidad de Costa Rica/[805-B0-810]/UCR/Costa RicaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)UCR::Vicerrectoría de Docencia::Ciencias Básicas::Facultad de Ciencias::Escuela de FísicaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigación en Ciencias del Mar y Limnología (CIMAR

Propuesta metodológica para la predicción climática estacional del veranillo en la cuenca del río Tempisque en el Pacífico Norte de Costa Rica

El ciclo anual de la precipitación en la vertiente del Pacífico de América Central, se caracteriza por tener dos máximos, uno entre mayo-junio y el otro entre setiembre-octubre, además de una estación seca de noviembre a abril y un periodo corto en el que las lluvias disminuyen durante julio-agosto, conocido como veranillo o canícula. En este trabajo se estudia la predictibilidad del veranillo, utilizando cuatro registros de precipitación diarios de las estaciones meteorológicas de Nicoya, Santa Cruz, Bagaces y Liberia, para el periodo 1937-2010 y localizadas en la cuenca del río Tempisque, provincia de Guanacaste, vertiente del Pacífico Norte de Costa Rica en América Central. Dentro de los aspectos considerados están la predictibilidad de la magnitud e intensidad del veranillo. Se explora la modulación de estos aspectos por fuentes de variabilidad climática asociadas con el Pacífico ecuatorial del Este (ENOS) y al océano Atlántico (AMO), incluyendo su variabilidad interanual y decenal. Cuando las anomalías normalizadas de ambos índices se comparan, se encontró que los eventos cálidos (fríos) del ENOS tienden a estar asociados con condiciones más (menos) secas durante el veranillo y estas condiciones se refuerzan cuando están asociados a su vez con condiciones de anomalías negativas (positivas) del AMO.On the Pacific slope of Central America, the precipitation annual cycle is characterized by two rainfall maxima in MayJune and September-October, an extended dry season from November to April, and a shorter reduced precipitation period during July-August known as Mid-Summer Drought (MSD) or “veranillo” and “canícula” in Spanish. Four daily gauge stations records, e.g. Nicoya, Santa Cruz, Liberia and Bagaces, located in the Tempisque river basin, province of Guanacaste, North Pacific slope of Costa Rica in Central America, were studied to explore the predictability of the MSD from 1937 to 2010. Among the aspects considered are the predictability of the MSD intensity and depth of the minimum. The modulation of these aspects by climate variability sources such as the Equatorial Eastern Pacific (ENSO) and the Atlantic Multidecadal Oscillation (AMO) was lately explored, including their interannual and decadal variability. When the normalized comparison is performed between the indices, it was found that warm (cool) ENSO events tend to be associated with dry (wet) MSD conditions and this condition is reinforced during periods with negative (positive) AMO anomalies.Universidad de Costa Rica/[805-B7-507]/UCR/Costa RicaUniversidad de Costa Rica/[805-B6-143]/UCR/Costa RicaUniversidad de Costa Rica/[805-B7-286]/UCR/Costa RicaUniversidad de Costa Rica/[805-B0-065]/UCR/Costa RicaUniversidad de Costa Rica/[805-A9-532]/UCR/Costa RicaUniversidad de Costa Rica/[805-A4-906]/UCR/Costa RicaUniversidad de Costa Rica/[805-B0-810]/UCR/Costa RicaUniversidad de Costa Rica/[805-B4-227]/UCR/Costa RicaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)UCR::Vicerrectoría de Docencia::Ciencias Básicas::Facultad de Ciencias::Escuela de FísicaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigación en Ciencias del Mar y Limnología (CIMAR