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Long- term changes in the CHl-a levels in the Black Sea Long- term changes in the CHl-a levels in the Black Sea
Illustration in a set of graphics prepared for a pilot assessment report on the Black Sea drainage basin, for the UNEP Global Impact on Waters Assessment (GIWA). All data and information were prepared in close collaboration with the GIWA Black Sea team and the GIWA secretariat. The graphics were not used in this form in the final report on the Black Sea, published in 2005.
07 Nov 2006 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Nutrients in the Varna Bay and the Romanian Black Sea costal area Nutrients in the Varna Bay and the Romanian Black Sea costal area
Illustration in a set of graphics prepared for a pilot assessment report on the Black Sea drainage basin, for the UNEP Global Impact on Waters Assessment (GIWA). All data and information were prepared in close collaboration with the GIWA Black Sea team and the GIWA secretariat. The graphics were never not used in this form in the final report on the Black Sea, published in 2005.
07 Nov 2006 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Fish catch in the Black Sea over the last 30 years Fish catch in the Black Sea over the last 30 years
Illustration in a set of graphics prepared for a pilot assessment report on the Black Sea drainage basin, for the UNEP Global Impact on Waters Assessment (GIWA). All data and information were prepared in close collaboration with the GIWA Black Sea team and the GIWA secretariat. The graphics were not used in this form in the final report on the Black Sea, published in 2005.
07 Nov 2006 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Monthly changes in the Danube discharge measured at the Ceatal Izmail station Monthly changes in the Danube discharge measured at the Ceatal Izmail station
Illustration in a set of graphics prepared for a pilot assessment report on the Black Sea drainage basin, for the UNEP Global Impact on Waters Assessment (GIWA). All data and information were prepared in close collaboration with the GIWA Black Sea team and the GIWA secretariat. The graphics were never not used in this form in the final report on the Black Sea, published in 2005.
10 Mar 2006 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Fish landings and fishing fleet in the Black Sea, 1975-1995 Fish landings and fishing fleet in the Black Sea, 1975-1995
Illustration in a set of graphics prepared for a pilot assessment report on the Black Sea drainage basin, for the UNEP Global Impact on Waters Assessment (GIWA). All data and information were prepared in close collaboration with the GIWA Black Sea team and the GIWA secretariat. The graphics were never not used in this form in the final report on the Black Sea, published in 2005.
07 Nov 2006 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Species diversity in the world's seas Species diversity in the world's seas
The graphic compares the amount of diversity of marine mammals, sharks, molluscs, birds, shrimp and lobsters in various sea regions. Coral reefs are among the most productive and diverse of all natural ecosystems. Recent decades have been catastrophic for them, however; some 10% of the world’s reefs may already have been degraded beyond recovery, and another 30% are in decline. Meanwhile biologically rich coastal wetlands, including mangrove fore...
28 Sep 2005 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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The decrease of Arctic sea ice, minimum extent in 1982 and 2007, and climate projections [Norwegian] The decrease of Arctic sea ice, minimum extent in 1982 and 2007, and climate projections [Norwegian]
Sattelite observations of the september extent of sea ice in the Arctic shows in 2007 shows a 23% decrease from the previous minimum, in 2005, and 39% below the average minimum extent for the time period 1979-2000. The bottom part of this graphic shows the development according to the Arctic Climate Impact Assessment (ACIA) and the merging of five global climate models - the resultant projections shows sucessive decreases for this century. The Ar...
28 Sep 2005 - by Hugo Ahlenius, UNEP/GRID-Arendal
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Coastal Arctic food web (drift ice) Coastal Arctic food web (drift ice)
The coastal Arctic food web is closely related to drift ice conditions and seasonal use of shorelines by both terrestrial and sea mammals. Numerous species depend upon each other and the transport of food to and from the marine areas to the coast and inland. Indigenous peoples use most of the food chain and traditionally use both environments for hunting, fishing and gathering.
28 Sep 2005 - by UNEP/GRID-Arendal
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The decrease of Arctic sea ice, minimum extent in 1982 and 2007, and climate projections The decrease of Arctic sea ice, minimum extent in 1982 and 2007, and climate projections
Sattelite observations of the september extent of sea ice in the Arctic shows in 2007 shows a 23% decrease from the previous minimum, in 2005, and 39% below the average minimum extent for the time period 1979-2000. The bottom part of this graphic shows the development according to the Arctic Climate Impact Assessment (ACIA) and the merging of five global climate models - the resultant projections shows sucessive decreases for this century. The Ar...
01 Dec 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
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Global International Waters Assessment (GIWA) case studies Global International Waters Assessment (GIWA) case studies
The Global International Waters Assessment (GIWA) is an example of a comprehensive strategic assessment designed to identify priorities for remedial and mitigatory actions in international waters. This graphic shows GIWA case studies for the Black Sea, the Amazon, the Great Barrier Reef and the Agulhas Current. Each case study includes an introduction and maps of the region and a discussion of the issues of concern for that region, such as freshw...
17 May 2005 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Aral Sea: trends and scenarios Aral Sea: trends and scenarios
The demise of the Aral Sea was caused primarily by the diversion of the inflowing Amu Dar'ya and Syr Dar'ya rivers to provide irrigation water for local croplands. This graphic shows the disappearance of the Aral Sea from 1957 to 2000 and three possible scenarios showing the relationship between future demand (and thus water abstraction) and future available runoff in cubic kilometres per year. The scenarios cover the time period from 2000 to 202...
17 May 2005 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Sea level change: estimations and predictions Sea level change: estimations and predictions
This resource includes four graphics that explain sea level change, an expected consequence of climate change. The first graphic, 'Relative Sea Level Over the Past 300 Years', shows the changes in sea level rise, in metres, that have occurred between 1700 and 2000 at three different locations: Amsterdam, Brest and Swinoujscie (in Poland). The second graphic, 'Causes of Sea Level Change: Simulated Global Mean Sea Level Changes 1900-2100' and the t...
17 May 2005 - by UNEP/GRID-Arendal
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Causes of sea level rise from climate change Causes of sea level rise from climate change
A significant sea level rise is one of the major anticipated consequences of climate change. This graphic explains the causes of sea level change according to the Intergovernmental Panel on Climate Change (IPCC). It explains the IPCC's A1 scenario family, which consists of three scenarios on future use of fossil energy sources, including scenario A1F1, which involves the use of fossil-intensive energy sources. This resource also includes the grap...
17 May 2005 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Shrinking of the Aral Sea: socio-economic impacts Shrinking of the Aral Sea: socio-economic impacts
Over the past 30 years, the Aral Sea in the former Soviet Union has shrunk to less than half of its original size. This graphic shows the Aral Sea as it was in 1960 and as it appeared in 2001. It shows that a former fishing zone is now a dry zone affected by salination. Areas that were previously food crops (partly irrigated) are now cotton and rice crops, widely irrigated. Other changes include the replacement of fish exports with fish imports, ...
17 May 2005 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Barents Region, topography and bathymetry Barents Region, topography and bathymetry
The Barents Region is in the Arctic and covers the area of Western Russia and the northern areas of Finland, Sweden and Norway. The Barents Sea has anaverage depth 230 m, bordered by the shelf edge towards the Norwegian Sea in the west, the island of Svalbard (Norway) in the northwest, and the islands of Franz Josef Land and Novaya Zemlya (Russia) in the northeast and east.
01 Jul 2006 - by Hugo Ahlenius, UNEP/GRID-Arendal
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Barents Region, topography and bathmetry Barents Region, topography and bathmetry
The Barents region is in the Arctic and covers the area of Western Russia and the northern areas of Finland, Sweden and Norway. The Barents Sea has an average depth 230 m, bordered by the shelf edge towards the Norwegian Sea in the west, the island of Svalbard (Norway) in the northwest, and the islands of Franz Josef Land and Novaya Zemlya (Russia) in the northeast and east. (Please note that the The Barents Euro-Arctic Council has expanded the m...
04 Oct 2005 - by Philippe Rekacewicz, UNEP/GRID-Arendal
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Arctic, topography and bathymetry (topographic map) Arctic, topography and bathymetry (topographic map)
The Arctic is extremely diverse in terms of landscapes, varying from pack and drift ice to rugged shores, flat coastal plains, rolling hills and mountains surpassing 6000 metres above sea level (Denali, 6,194 m asl, in sub-arctic and boreal Alaska). The region has rivers and lakes, tundra and the largest forests in the world (the Russian Taiga).
04 Oct 2005 - by Hugo Ahlenius, UNEP/GRID-Arendal
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Arctic, topography and bathymetry Arctic, topography and bathymetry
(See http://maps.grida.no/go/graphic/arctic-topography-and-bathymetry1 for an updated version of this map) The Arctic is extremely diverse in terms of landscapes, varying from pack and drift ice to rugged shores, flat coastal plains, rolling hills and mountains surpassing 6000 metres above sea level (Denali, 6,194 m asl, in sub-arctic and boreal Alaska). The region has rivers and lakes, tundra and the largest forests in the world (the Russian Tai...
04 Oct 2005 - by Hugo Ahlenius, UNEP/GRID-Arendal
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Moldova, topographic map Moldova, topographic map
Moldova is located in Eastern Europe, northeast of Romania, comprising of 33,843 sq km. It has a population of 4,455,421 (2005). Major environmental concerns are: heavy use of agricultural chemicals, including banned pesticides such as DDT, has contaminated soil and groundwater; extensive soil erosion from poor farming methods.
04 Oct 2005 - by Philippe Rekacewicz, Emmanuelle Bournay, UNEP/GRID-Arendal
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Barents Region, topography and bathymetry Barents Region, topography and bathymetry
The Barents Region is in the Arctic and covers the area of Western Russia and the northern areas of Finland, Sweden and Norway. The Barents Sea has anaverage depth 230 m, bordered by the shelf edge towards the Norwegian Sea in the west, the island of Svalbard (Norway) in the northwest, and the islands of Franz Josef Land and Novaya Zemlya (Russia) in the northeast and east.
01 Jul 2006 - by Hugo Ahlenius, UNEP/GRID-Arendal
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