Global war : the Second World War, 1939-1945.

La Segunda Guerra se divide en tres partes que describen la propagación de la guerra de Polonia al resto de Europa, su expansión a escala mundial y, finalmente, la guerra total que terminó con la derrota de las potencias del Eje en 1943-45. Incluye fragmentos de fuentes históricas originales, así como, material de aprendizaje activo: ejercicios, preguntas, y pruebas.

The age of excess : America 1920-1932.

Entre 1920 y 1932 Estados Unidos aumentó en gran medida su nivel de prosperidad y, a continuación, se estrelló en las profundidades de la depresión. América es la tierra de la oportunidad y su sistema democrático ofrece un sueño de libertad a pesar de los problemas raciales, la intolerancia política, la prohibición, los gangsters, la violencia y las diferencias religiosas. Estos años fueron los locos años veinte que terminaron con el Crash de 1929.Incluye fragmentos de fuentes históricas originales, así como, material de aprendizaje activo: ejercicios, preguntas y pruebas.

A New Deal : America 1932-1945.

En 1932 el Presidente Roosevelt prometió un New Deal para sacar a los Estados Unidos de la depresión. Consistió en la creación de planes orientados a los desempleados, a los campesinos, para la tierra y la industria. Se muestra cómo tuvo que enfrentarse a la oposición a estos planes y a la participación de su país en la Segunda Guerra Mundial. Por último, se repasan los juicios emitidos por los contemporáneos y valoraciones posteriores sobre su figura y su New Deal. Incluye fragmentos de fuentes históricas originales, así como, material de aprendizaje activo: ejercicios, preguntas, y pruebas.

Russia in war and revolution : Russia 1900-1924.

Se examinan las malas condiciones de vida en las que se encontraba la población rusa a principios del siglo XX, y lo poco que el gobierno zarista hizo para mejorarlas. Se describen los acontecimientos que llevaron a los bolcheviques al poder en 1917 y cómo Lenin obtuvo el control del país, introdujo una nueva política económica y una nueva constitución. Incluye fragmentos de fuentes históricas originales, así como, material de aprendizaje activo: ejercicios, preguntas, y pruebas.

Stalin and the Soviet Union : the USSR 1924-1953.

Los años 1924-1953 estuvieron dominados por la figura de Stalin, el culto a su figura y su lucha por el poder en el Partido Comunista. Se describen los planes quinquenales de desarrollo de la economía soviética, así como las purgas y los juicios de la década de 1930. Por último, se examina la manera en que la URSS reaccionó a la amenaza de los países capitalistas durante los años 1920 y 1930 y en la forma en que luchó por la supervivencia contra la Alemania nazi durante la segunda guerra mundial.Incluye fragmentos de fuentes históricas originales, así como, material de aprendizaje activo: ejercicios, preguntas, y pruebas.

The cold war : superpower relations, 1945-1989.

Desde el final de la Segunda Guerra Mundial y hasta 1990, las relaciones internacionales estuvieron dominadas por este peligroso conflicto, durante el cual tanto los países comunistas como no comunistas luchaban por el dominio del mundo. Para conseguirlo, desarrollaron armas nucleares de destrucción masiva. En varias ocasiones, esta amenaza de guerra fría se intensificó y, dio lugar a episodios críticos en diferentes países, que pudieron iniciar una tercera guerra. Incluye fragmentos de fuentes históricas originales, así como, material de aprendizaje activo: ejercicios, preguntas, y pruebas.

The response of tropospheric circulation to perturbations in lower-stratospheric temperature

A multiple regression analysis of the NCEP-NCAR reanalysis dataset shows a response to increased solar activity of a weakening and poleward shift of the subtropical jets. This signal is separable from other influences, such as those of El Nino-Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO), and is very similar to that seen in previous studies using global circulation models (GCMs) of the effects of an increase in solar spectral irradiance. The response to increased stratospheric (volcanic) aerosol is found in the data to be a weakening and equatorward shift of the jets. The GCM studies of the solar influence also showed an impact on tropospheric mean meridional circulation with a weakening and expansion of the tropical Hadley cells and a poleward shift of the Ferrel cells. To understand the mechanisms whereby the changes in solar irradiance affect tropospheric winds and circulation, experiments have been carried out with a simplified global circulation model. The results show that generic heating of the lower stratosphere tends to weaken the subtropical jets and the tropospheric mean meridional circulations. The positions of the jets, and the extent of the Hadley cells, respond to the distribution of the stratospheric heating, with low-latitude heating forcing them to move poleward, and high-latitude or latitudinally uniform heating forcing them equatorward. The patterns of response are similar to those that are found to be a result of the solar or volcanic influences, respectively, in the data analysis. This demonstrates that perturbations to the heat balance of the lower stratosphere, such as those brought about by solar or volcanic activity, can produce changes in the mean tropospheric circulation, even without any direct forcing below the tropopause.

Solar influences on dynamical coupling between the stratosphere and troposphere

We use a simplified atmospheric general circulation model (AGCM) to investigate the response of the lower atmosphere to thermal perturbations in the lower stratosphere. The results show that generic heating of the lower stratosphere tends to weaken the sub-tropical jets and the tropospheric mean meridional circulations. The positions of the jets, and the extent of the Hadley cells, respond to the distribution of the stratospheric heating, with low latitude heating displacing them poleward, and uniform heating displacing them equatorward. The patterns of response to the low latitude heating are similar to those found to be associated with solar variability in previous observational data analysis, and to the effects of varying solar UV radiation in sophisticated AGCMs. In order to investigate the chain of causality involved in converting the stratospheric thermal forcing to a tropospheric climate signal we conduct an experiment which uses an ensemble of model spin-ups to analyse the time development of the response to an applied stratospheric perturbation. We find that the initial effect of the change in static stability at the tropopause is to reduce the eddy momentum flux convergence in this region. This is followed by a vertical transfer of the momentum forcing anomaly by an anomalous mean circulation to the surface, where it is partly balanced by surface stress anomalies. The unbalanced part drives the evolution of the vertically integrated zonal flow. We conclude that solar heating of the stratosphere may produce changes in the circulation of the troposphere even without any direct forcing below the tropopause. We suggest that the impact of the stratospheric changes on wave propagation is key to the mechanisms involved.

Impact of Tibetan Orography and Heating on the Summer Flow over Asia

The influence on the summer flow over Asia of both the orographic and thermal forcing of the Tibetan Plateau is investigated using a sequence of idealised experiments with a global primitive equation model. The zonally averaged flow is prescribed and both realistic and idealised orography and heating are used. There is some similarity between the responses to the two forcings when applied separately. The upper tropospheric Tibetan anticyclone is predominantly forced by the heating but also weakly by the orography. Below this, both forcings tend to give air descending in an equatorward anticyclonic circulation down the isentropes to the west and rising in a similar poleward circulation to the east. However the heating-only response has a strong ascending southwesterly flow that is guided around the south and south-east of the orography when it is included. On the northern side, the westerly flow over the orography gives ascent on the upslope and descent on the downslope. It is found that heating over the Plateau leads to a potential vorticity (PV) minimum and that if it is sufficiently strong the flow is unstable, producing a quasi-biweekly oscillation. During this oscillation the Tibetan anticyclone changes between a single centre over the southwestern side of the Plateau and a split/double structure with centres over China and the Middle East. These characteristics are similar to observed variability in the region. Associated with this quasi-biweekly oscillation are significant variations in the strength of the ascent over the Plateau and the Rossby wave pattern over the North Pacific. The origin of the variability is instability associated with the zonally extended potential vorticity PV minimum on a θ-surface, as proposed by Hsu and Plumb (2000). This minimum is due to the tendency to reduce the PV above the heating over the Plateau and to advection by the consequent anticyclone of high PV around from the east and low PV to the west. The deep convection to the south and southeast of the Plateau tends to suppress the quasi-biweekly oscillation because the low PV produced above it acts to reduce the meridional PV gradient reversal. The occurrence of the oscillation depends on the relative magnitude of the heating in the two regions.

A new Rossby Wave-breaking interpretation of the North Atlantic Oscillation

This paper proposes the hypothesis that the low-frequency variability of the North Atlantic Oscillation (NAO) arises as a result of variations in the occurrence of upper-level Rossby wave–breaking events over the North Atlantic. These events lead to synoptic situations similar to midlatitude blocking that are referred to as high-latitude blocking episodes. A positive NAO is envisaged as being a description of periods in which these episodes are infrequent and can be considered as a basic, unblocked situation. A negative NAO is a description of periods in which episodes occur frequently. A similar, but weaker, relationship exists between wave breaking over the Pacific and the west Pacific pattern. Evidence is given to support this hypothesis by using a two-dimensional potential-vorticity-based index to identify wave breaking at various latitudes. This is applied to Northern Hemisphere winter data from the 40-yr ECMWF Re-Analysis (ERA-40), and the events identified are then related to the NAO. Certain dynamical precursors are identified that appear to increase the likelihood of wave breaking. These suggest mechanisms by which variability in the tropical Pacific, and in the stratosphere, could affect the NAO.

The Storm-Track Response to Idealized SST Perturbations in an Aquaplanet GCM

The tropospheric response to midlatitude SST anomalies has been investigated through a series of aquaplanet simulations using a high-resolution version of the Hadley Centre atmosphere model (HadAM3) under perpetual equinox conditions. Model integrations show that increases in the midlatitude SST gradient generally lead to stronger storm tracks that are shifted slightly poleward, consistent with changes in the lower-tropospheric baroclinicity. The large-scale atmospheric response is, however, highly sensitive to the position of the SST gradient anomaly relative to that of the subtropical jet in the unperturbed atmosphere. In particular, when SST gradients are increased very close to the subtropical jet, then the Hadley cell and subtropical jet is strengthened while the storm track and eddy-driven jet are shifted equatorward. Conversely, if the subtropical SST gradients are reduced and the midlatitude gradients increased, then the storm track shows a strong poleward shift and a well-separated eddy-driven jet is produced. The sign of the SST anomaly is shown to play a secondary role in determining the overall tropospheric response. These findings are used to provide a new and consistent interpretation of some previous GCM studies concerning the atmospheric response to midlatitude SST anomalies.

Large-scale context for the UK floods in summer 2007

This paper shows how the rainfall distribution over the UK, in the three major events on 13-15 June, 25 June and 20 July 2007, was related to troughs in the upper-level flow, and investigates the relationship of these features to a persistent large-scale flow pattern which extended around the northern hemisphere and its possible origins. Remote influences can be mediated by the propagation of large-scale atmospheric waves across the northern hemisphere and also by the origins of the air-masses that are wrapped into the developing weather systems delivering the rain to the UK. These dynamical influences are examined using analyses and forecasts produced by a range of atmospheric models.