Spread of low-cost carriers : tourism and regional policy effects in Spain
Aéroport ; Développement urbain ; Espagne ; Mobilité ; Politique régionale ; Tourisme ; Transport ; Transport aérien ; Transport low-cost
La configuration des nouvelles relations ligne aérienne-aéroport-intégration régionale. L'impact du trafic low-cost sur le réseau des aéroports espagnols. Les effets des opérations de transporteurs low-cost sur l'activité touristique. Tourisme et
politiques régionales en Espagne : une synthèse de l'évolution. Tourisme et politiques de développement régional en liaison avec les transporteurs low-cost.
Fluvial adjustment of the Lower Jordan River to a drop in the Dead Sea level
This paper examines the effects of base level lowering on the channel morphology of the southern end of the Lower Jordan River. The recent chronology and rate of channel changes through the lower reach of the river caused by the lowering of the base
River sedimentation and channel adjustment of the lower Yellow River as influenced by low discharges and seasonal channel dry-ups
Fluvial sedimentation can be classified as one of the 3 types in terms of different morphological units, i.e., vertical overbank deposition, vertical deposition on the riverbed and lateral deposition on the riverbank. With the example of the lower
Yellow River, the 3 types of sedimentation have been studied in relation to channel adjustment, emphasizing the changes under the conditions of low discharge and seasonal desiccations since 1986.
These unions are financial co-operatives based on low-income neighbourhoods, owned and controlled by local residents. Although located in economically disadvantaged communities, they are not exclusively used by the poor, and are making useful
but marginal contributions to the credit and debt problems of low-income families in Great Britain.
Impact of flow variability on the morphology of a low-energy meandering river
This paper examines the impact of sequential flows of various magnitudes on the morphology of a low-energy river in northeastern Illinois. Between June 1986 and November 1988, the measurement programme has thus far bracketed extreme as well
as moderate events and the data elucidate the short-term fluvial dynamics of the low-energy meandering Des Plaines river.
Privatisation of housing and the impact of the Conservative Government's initiatives on low-cost homeownership and private renting between 1979 and 1984 in England and Wales | 2. implementation of low-cost homeownership policy
Privatisation of housing and the impact of the Conservative Government's initiatives on low-cost homeownership and private renting between 1979 and 1984 in England and Wales : 3. Impact and evaluation of low-cost homeownership policy
Morphometry and morphodynamics of the lower Vistula channel mesoforms
The objective of this study is to determine the morphometry and morphodynamics of the prevailing mesoforms of the lower Vistula channel, i.e. unsteady movement of load. In view of the fact that these forms are the resultant of load movement
Relatively low activities of the Hokkaido economy and regional development strategies
Some factors in the relatively low activity of the Hokkaido economy and regional development policies. The improvement of those factors, especially using the strategies for adding higher value to products of primary industry. - (SGA)
Holocene surface lowering in the Lias cuesta area of Luxembourg as calculated from the amount of volcanic minerals of Allerod age remaining in residual soils
A method is given for calculating the surface lowering of residual soils in Luxembourg from the amount of volcanic minerals surviving holocene erosion after their deposition at the end of the Pleistocene. The amount of lowering equals the depth
of soil homogenisation multiplied by the natural logarithm of the ratio between the original and the present frequency of the volcanic minerals. With this method it is shown that the probable lowering of the Lias cuesta by holocene soil erosion ranges from
0 to 57cm the maximum lowering occuring on the steep lower part of the escarpment slope underlain by the fine-grained Keuper soils.