The importance of institutions in expansionary fiscal consolidations. A critical assessment of non-Keynesian effects

The short-term effects of fiscal consolidation have attracted an increasing attention from both the academia and policy makers in the recent years. Authors in the literature on non- Keynesian effects usually put the emphasis on the need for the devaluation of the national currency, the accommodating reaction of the monetary authority and the favourable international economic conditions as the necessary accompanying tools of fiscal consolidation, in order to realise short-term expansionary effects. Some also add the necessity of large-scale adjustment; while others support the view that a high and increasing debt ratio or increasing government spending, by triggering an unavoidable adjustment, is the key to experiencing short-term expansionary effects. The composition of adjustment also became a crucial explanation for non-Keynesian effects. However, as the following critical assessment of the literature on expansionary fiscal consolidations will reveal, institutional conditions, such as the importance of the depth of financial intermediation and the influencing role of labour market structure, can prove to be crucial in the occurrence of the desired expansionary short-term effects.

Modelling the growth of young individuals of Pinus nigra on thin carbonate soils under climate change in Hungary

Climate change highly impacts on tree growth and also threatens the forest of the karstic terrains. From the 1980s the frequency of decay events of the Pinus nigra Arnold forests showed a marked increase in Hungary. To understanding the vulnerability of Pinus nigra forests to climate change on shallow karstic soils in continental-sub Mediterranean climatic conditions we developed the study of three sampled population in the typical karstic landscape of Veszprém in North Transdanubia. We built our model on non-invasive approach using the annual growth of the individuals. MPI Echam5 climate model and as aridity index the Thornthwaite Agrometeorological Index were used. Our results indicate that soil thickness up to 11 cm has a major influence on the main growth intensity, however, aridity determines the annual growth rate. Our model results showed that the increasing decay frequency in the last decades was a parallel change to the decreasing growth rate of pines. The climate model predicts the similar, increased decay frequency to the presents. Our results can be valid for a wider areas of the periphery of Mediterranean climate zone while the annual-growth based model is a cost-effective and simple method to study the vitality of pine trees in a given area.