20 research outputs found
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Effect of Surface Heterogeneity on the Boundary-Layer Height: A Case Study at a Semi-Arid Forest
We investigate the effects of an isolated meso-Ī³-scale surface heterogeneity for roughness and albedo on the atmospheric boundary-layer (ABL) height, with a case study at a semi-arid forest surrounded by sparse shrubland (forest area: 28km2, forest length in the main wind direction: 7 km). Doppler lidar and ceilometer measurements at this semi-arid forest show an increase in the ABL height over the forest compared with the shrubland on four out of eight days. The differences in the ABL height between shrubland and forest are explained for all days with a model that assumes a linear growth of the internal boundary layer of the forest through the convective ABL upwind of the forest followed by a square-root growth into the stable free atmosphere. For the environmental conditions that existed during our measurements, the increase in ABL height due to large sensible heat fluxes from the forest (600Wm-2 in summer) is subdued by stable stratification in the free atmosphere above the ABL, or reduced by high wind speeds in the mixed layer
Recommended from our members
Effect of Surface Heterogeneity on the Boundary-Layer Height: A Case Study at a Semi-Arid Forest
We investigate the effects of an isolated meso-Ī³-scale surface heterogeneity for roughness and albedo on the atmospheric boundary-layer (ABL) height, with a case study at a semi-arid forest surrounded by sparse shrubland (forest area: 28km2, forest length in the main wind direction: 7 km). Doppler lidar and ceilometer measurements at this semi-arid forest show an increase in the ABL height over the forest compared with the shrubland on four out of eight days. The differences in the ABL height between shrubland and forest are explained for all days with a model that assumes a linear growth of the internal boundary layer of the forest through the convective ABL upwind of the forest followed by a square-root growth into the stable free atmosphere. For the environmental conditions that existed during our measurements, the increase in ABL height due to large sensible heat fluxes from the forest (600Wm-2 in summer) is subdued by stable stratification in the free atmosphere above the ABL, or reduced by high wind speeds in the mixed layer
THE POLITICS OF MICROPOLICY: INNOVATION AND INDUSTRIAL POLICY IN THE UNITED STATES
The author compares the origins and prominence of efforts in the U.S. to initiate innovation policy and industrial policy. Efforts to develop innovation policy have proven t o be obscure, episodic, relatively noncontroversial, and confined to a narrow political arena. They typically resulted in short-lived spending programs. In contrast, in less than four years the industrial policy proposals introduced have been far more ambitious, generated broad interest groups support and opposition, and sparked vigorous, widely publicized controversy. These differences cannot be explained by differences in analytical difficulties or in the uncertainty of benefits derived. They derive from the failure and success of the two issues to engage politically active constituencies and from the corresponding roles of Congress and the bureaucracy. Copyright 1984 by The Policy Studies Organization.