‘Sudden Stratospheric Warming and its Influence on the Tropical Atmosphere'

The stratospheric warming events are categorized into major and minor warming depending on the temperature increase in the polar stratosphere. The warming is called a ‘major’, when the polar temperature increases poleward from 60 degree latitude and followed by a reversal in the zonal wind at 10 hPa (~32 Km). Usually major warming events are associated with the displacement of polar vortex from high to mid latitudes or the splitting of vortices in to two. The warming is called a "Minor", when the polar temperature increases more than 25 degree in a period of a week or less, at any stratospheric level with less intensified easterly wind anomalies. The stratospheric warmings generated during the transition period of winter to spring are called final warmings. The warming events observed in the early winter period (November to early December) over Canadian region are called Canadian warmings. There is strong interaction between stratosphere and troposphere during SSW period over high and low latitudes regions. The thesis consists of 7 chapters

Storms : causes and effects.

En esta serie los jóvenes lectores se acercan a los diferentes tipos de clima que experimentamos en la Tierra. Además de tratar el tema de un fenómeno meteorológico en particular, se incluye información sobre el pronostico del tiempo y vemos, además, las formas en que las personas, los animales y las plantas modifican su comportamiento de acuerdo a determinadas condiciones meteorológicas.

Latitude and longitude.

Se estudia la historia de la cartografía y su relación con las exploraciones, la navegación y la medición del tiempo. El descubrimiento de tierras, océanos y pueblos se produjo hacia 1500 cuando los europeos, sin acceso a las rutas comerciales de China y del Lejano Oriente, debían cruzar los océanos para llegar a sus mercados.

Mid-Tudor crises, 1536-69.

Cumple con los requisitos para la especificación OCR AS de Historia, unidad F963, opción A, tema 2 'Investigaciones'. Se divide en cinco capítulos: introducción al período histórico, valoración de la estabilidad de la monarquía, significación de los cambios religiosos de la época, los efectos del cambio social y económico y la naturaleza del desafío a la autoridad real. Cada capítulo contiene actividades para ayudar a la comprensión del tema y desarrollar habilidades con la historia, breves biografías de personajes clave de la época y vocabulario nuevo, análisis de acontecimientos relevantes, de debates y controversias y consejos para los exámenes.

Mid-term Evaluation of the 2009-14 European Parliament: Legislative activity and decision-making dynamics. CEPS Special Report, 23 July 2012

This special report analyses legislative activity in the European Union and coalition formation in the European Parliament (EP) during the first half of the 7th legislative term, 2009-14. Co-decision is now the ordinary legislative procedure, not by name only: it was deployed on 90% of new proposals in 2010 and 86% in 2011, which suggests that the EP is now more influential than ever. There are differences in the degree of empowerment across committees, however. This report looks at the legislative workload of selected committees as an indicator of change in their influence, identifying which of them won and which lost out in terms of the quantity and type of legislation they tackle.

Piping Plover response to coastal storms occurring during the nonbreeding season

The increase in coastal storm frequency and intensity expected under most climate change scenarios is likely to substantially modify beach configuration and associated habitats. This study aimed to analyze the impact of coastal storms on a nesting population of the endangered Piping Plover (Charadrius melodus melodus) in southeastern New Brunswick, Canada. Previous studies have shown that numbers of nesting Piping Plovers may increase following storms that create new nesting habitat at individual beaches. However, to our knowledge, no test of this pattern has been conducted over a regional scale. We hypothesized that Piping Plover abundance would increase after large coastal storms occurring during the nonbreeding season. However, we expected a delay in the colonization of newly created habitat owing to low-density populations, combined with high site fidelity of adults and high variability in survival rate of subadults. We tested this hypothesis using a 27-year (1986-2012) data set of Piping Plover abundance and productivity (nesting pairs and fledged young) collected at five sites in eastern New Brunswick. We identified 11 major storms that could potentially have modified Piping Plover habitat over the study period. The number of fledged young increased three years after a major storm, but the relationship was much weaker for the number of nesting pairs. These findings are consistent with the hypothesized increase in suitable habitat after coastal storms. Including storm occurrence with other factors influencing habitat quality will enhance Piping Plover conservation strategies.

Chemical composition observed over the mid-Atlantic and the detection of pollution signatures far from source regions

The atmospheric composition of the central North Atlantic region has been sampled using the FAAM BAe146 instrumented aircraft during the Intercontinental Transport of Ozone and Precursors (ITOP) campaign, part of the wider International Consortium for Atmospheric Research on Transport and Transformation (ICARTT). This paper presents an overview of the ITOP campaign. Between late July and early August 2004, twelve flights comprising 72 hours of measurement were made in a region from approximately 20 to 40°W and 33 to 47°N centered on Faial Island, Azores, ranging in altitude from 50 to 9000 m. The vertical profiles of O3 and CO are consistent with previous observations made in this region during 1997 and our knowledge of the seasonal cycles within the region. A cluster analysis technique is used to partition the data set into air mass types with distinct chemical signatures. Six clusters provide a suitable balance between cluster generality and specificity. The clusters are labeled as biomass burning, low level outflow, upper level outflow, moist lower troposphere, marine and upper troposphere. During this summer, boreal forest fire emissions from Alaska and northern Canada were found to provide a major perturbation of tropospheric composition in CO, PAN, organic compounds and aerosol. Anthropogenic influenced air from the continental boundary layer of the USA was clearly observed running above the marine boundary layer right across the mid-Atlantic, retaining high pollution levels in VOCs and sulfate aerosol. Upper level outflow events were found to have far lower sulfate aerosol, resulting from washout on ascent, but much higher PAN associated with the colder temperatures. Lagrangian links with flights of other aircraft over the USA and Europe show that such signatures are maintained many days downwind of emission regions. Some other features of the data set are highlighted, including the strong perturbations to many VOCs and OVOCs in this remote region.