972 resultados para Alcuin, 735-804.


Report drawn up on behalf of the Committeeon Agriculture on A. the proposals from the Commission of the European Communities to the Council (Doc. 1-893/83-COM(83) 548 final) for: I. a regulation amending Regulation (EEC) No. 804/68 on the common organization of the markets in milk and milk products. II. a regulation laying down general rules applying to the milk sector levy specified in Article 5(c) of Regulation (EEC) No. 804/68. III. a regulation laying down general rules applying to the milk sector levy specified in Article 5(d) of Regulation (EEC) No. 804/68. B. the proposals from the Commission of the European Communities to the Council (Doc. 1-996/83-COM(83) 611 final) for: I. a regulation amending Regulation (EEC No. 1723/81 as regards the possibility of granting aids for the use of butter in the manufacture of certain food-stuffs. II. a regulation amending Regulation (EEC) No. 1411/71 as regards the fat content of drinking milk. III. a regulation laying down general rules on the granting of aid for concentrated skimmed milk and concentrated milk for use as animal feed. IV. a regulation amending Regulation (EEC) No. 1269/79 with regard to the terms for the disposal of butter at a reduced price for direct consumption. C. the proposal from the Commission of the European Communities to the Council (Doc. 1-1113/83)-COM(83) 644 final) for a regulation amending Regulations (EEC) No. 1078/77 introducing a system of premiums for the non-marketing of milk and milk products and for the conversion of dairy herds.

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Arctic sea ice has declined and become thinner and younger (more seasonal) during the last decade. One consequence of this is that the surface energy budget of the Arctic Ocean is changing. While the role of surface albedo has been studied intensively, it is still widely unknown how much light penetrates through sea ice into the upper ocean, affecting sea-ice mass balance, ecosystems, and geochemical processes. Here we present the first large-scale under-ice light measurements, operating spectral radiometers on a remotely operated vehicle (ROV) under Arctic sea ice in summer. This data set is used to produce an Arctic-wide map of light distribution under summer sea ice. Our results show that transmittance through first-year ice (FYI, 0.11) was almost three times larger than through multi-year ice (MYI, 0.04), and that this is mostly caused by the larger melt-pond coverage of FYI (42 vs. 23%). Also energy absorption was 50% larger in FYI than in MYI. Thus, a continuation of the observed sea-ice changes will increase the amount of light penetrating into the Arctic Ocean, enhancing sea-ice melt and affecting sea-ice and upper-ocean ecosystems.

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Mode of access: Internet.

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Description based on: 93-012 (Aug. 1993); title from cover.