research proposal ikea in the loop of Indian market

prospect of Ikea considering Indian market

Oceans Deep: Lesson G (March of The Polar Bears)

Teacher resources for Lesson G in the Discover Oceanography 'Scheme of Work' for use in schools.

Oceans Deep: Lesson A (The ocean conveyor belt)

Teacher resources for Lesson G in the Discover Oceanography 'Scheme of Work' for use in schools.

Oceans and rivers.

Con un formato de pregunta y respuesta se presenta la información acerca de los océanos, ríos, islas, arrecifes, corrientes oceánicas, aguas subterráneas, grandes lagos, y cómo se formaron. Trata de despertar la curiosidad para profundizar en su estudio y el respeto por su conservación.

Oceans.

Mapas,diagramas, experimentos, los modelos de paisajes, ayudan a los niños a comprender los conceptos de las ciencias de la Tierra. Para tratar de entender cómo se mueve el agua de mar en todo el mundo, cómo los océanos se formaron y qué efectos tienen en las costas.

The effect of doubled CO2 and model basic state biases on the monsoon-ENSO system. II: Changing ENSO regimes

Integrations of a fully-coupled climate model with and without flux adjustments in the equatorial oceans are performed under 2×CO2 conditions to explore in more detail the impact of increased greenhouse gas forcing on the monsoon-ENSO system. When flux adjustments are used to correct some systematic model biases, ENSO behaviour in the modelled future climate features distinct irregular and periodic (biennial) regimes. Comparison with the observed record yields some consistency with ENSO modes primarily based on air-sea interaction and those dependent on basinwide ocean wave dynamics. Simple theory is also used to draw analogies between the regimes and irregular (stochastically forced) and self-excited oscillations respectively. Periodic behaviour is also found in the Asian-Australian monsoon system, part of an overall biennial tendency of the model under these conditions related to strong monsoon forcing and increased coupling between the Indian and Pacific Oceans. The tropospheric biennial oscillation (TBO) thus serves as a useful descriptor for the coupled monsoon-ENSO system in this case. The presence of obvious regime changes in the monsoon-ENSO system on interdecadal timescales, when using flux adjustments, suggests there may be greater uncertainty in projections of future climate, although further modelling studies are required to confirm the realism and cause of such changes.