MICROBIOLOGICAL INDICATORS FOR MONITORING MARINE POLLUTION IN THE BALTIC SEA AND THE MEDITERRANEAN SEA

Author(s):  
H. Dizer ◽  
P.-D. Hansen
Author(s):  
Eric Schnakenbourg

In the Early Modern era, the Baltic Sea was called the Nordic Mediterranean because of its unique outlet on the high seas and its narrowness. Like its southern counterpart, the Baltic is at the crossroads of several peoples and cultures. Also like the Mediterranean Sea, the Baltic had different populations on each of its shores, yet in another way facilitated relations and became a space for interconnections. Throughout its history, peoples from Scandinavia, Poland, Germany, Russia, and the Baltic lands developed not only all sorts of peaceful relations and exchanges, but also competed with each other in long-lasting rivalries or military confrontations. Between the 16th century and the first half of the 19th century, the Baltic region experienced dramatic internal and external changes resulting from its ever-growing connections with the rest of Europe. Baltic issues, however, did not have the same importance for all the surrounding countries: it was the only horizon for Sweden, which enjoyed sovereignty over Finland until 1809, and the main horizon for Denmark, which ruled Norway until 1814. For Scandinavians, the Baltic Sea was a necessary interface for various kinds of exchanges with the external world, whether regional neighbors or continental Europe. In one way or another, the history of the Swedish and Danish kingdoms is interwoven with the history of the Baltic. Scandinavians devoted great attention to this neighboring sea for their shipping and trade, as well as for their security and political influence. The situation is somewhat similar for the Baltic provinces (Estonia, Livonia, and Ingria), which were always under foreign rule, first Swedish then Russian, in the Early Modern period. On the other side of the sea, for the German states, the Polish Republic, and the Russian Empire, the Baltic was simply one theater of foreign policy among others, even though its importance changed over time according to the political or economic context. As for commerce, while during the Middle Ages the Baltic region traded with the rest of Europe, starting in the 16th century, the situation changed as the continental economy shifted from the Mediterranean to the northwest. European population growth and the development of long-distance shipping and commerce meant increasing needs for grain and naval stores. This created new demand for Baltic economic resources and products and for transporting those exports. Consequently, new international rivalries and struggles occurred in the Baltic. At first, these conflicts were among the regional countries, but increasingly the main European powers as well. The Baltic Sea then became an important theater for European international politics, and almost every continental war had a Baltic component. The history of the Baltic Sea from the 16th century to the middle of the 19th century must be considered from two perspectives: first, relations among the regional countries and peoples; and second, relations with the world outside the Baltic, whether foreign powers and regions or even other seas, for political, military, and trade matters.


2021 ◽  
Vol 21 (7) ◽  
pp. 5477-5498
Author(s):  
Maxi Boettcher ◽  
Andreas Schäfler ◽  
Michael Sprenger ◽  
Harald Sodemann ◽  
Stefan Kaufmann ◽  
...  

Abstract. Warm conveyor belts (WCBs) are important airstreams in extratropical cyclones, often leading to the formation of intense precipitation and the amplification of upper-level ridges. This study presents a case study that involves aircraft, lidar and radar observations in a WCB ascending from western Europe towards the Baltic Sea during the Hydrological Cycle in the Mediterranean Experiment (HyMeX) and T-NAWDEX-Falcon in October 2012, a preparatory campaign for the THORPEX North Atlantic Waveguide and Downstream Impact Experiment (T-NAWDEX). Trajectories were used to link different observations along the WCB, that is, to establish so-called Lagrangian matches between observations. To this aim, an ensemble of wind fields from the global analyses produced by the European Centre for Medium-Range Weather Forecasts (ECMWF) Ensemble of Data Assimilations (EDA) system were used, which allowed for a probabilistic quantification of the WCB occurrence and the Lagrangian matches. Despite severe air traffic limitations for performing research flights over Europe, the German Aerospace Center (DLR) Falcon successfully sampled WCB air masses during different phases of the WCB ascent. The WCB trajectories revealed measurements in two distinct WCB branches: one branch ascended from the eastern North Atlantic over southwestern France, while the other had its inflow in the western Mediterranean. Both branches passed across the Alps, and for both branches Lagrangian matches coincidentally occurred between lidar water vapour measurements in the inflow of the WCB south of the Alps, radar measurements during the ascent at the Alps and in situ aircraft measurements by Falcon in the WCB outflow north of the Alps. An airborne release experiment with an inert tracer could confirm the long pathway of the WCB from the inflow in the Mediterranean boundary layer to the outflow in the upper troposphere near the Baltic Sea several hours later. The comparison of observations and ensemble analyses reveals a moist bias in the analyses in parts of the WCB inflow but a good agreement of cloud water species in the WCB during ascent. In between these two observations, a precipitation radar measured strongly precipitating WCB air located directly above the melting layer while ascending at the southern slopes of the Alps. The trajectories illustrate the complexity of a continental and orographically influenced WCB, which leads to (i) WCB moisture sources from both the Atlantic and Mediterranean, (ii) different pathways of WCB ascent affected by orography, and (iii) locally steep WCB ascent with high radar reflectivity values that might result in enhanced precipitation where the WCB flows over the Alps. The linkage of observational data by ensemble-based WCB trajectory calculations, the confirmation of the WCB transport by an inert tracer and the model evaluation using the multi-platform observations are the central elements of this study and reveal important aspects of orographically modified WCBs.


Author(s):  
C. J. Webb

The common goby, Pomatoschistus microps (Krøyer), is a small, euryhaline gobiid fish which ranges along the coasts of continental Europe from the Mediterranean to Trondheim, Norway, and also penetrates into the Baltic Sea (Miller, 1973). This species, which can be very abundant, is generally distributed in estuaries, salt marsh and shore pools (Wheeler, 1969; Miller, 1971) and experiences a higher degree of environmental heterogeneity than most of the other European gobiids (Wallis & Beardmore, 1984a).


Author(s):  
Vladimir Zalesny ◽  
Anatoly Gusev ◽  
Sergey Chernobay ◽  
Robert Aps ◽  
Rein Tamsalu ◽  
...  

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