Invigorating the United Nations Global Programme of Action (GPA) for the Protection of the Marine Environment from Land-Based Activities––utilizing both bottom-up and top-down approaches

2002 ◽  
Vol 44 (8) ◽  
pp. 719-721
Author(s):  
Peter G. Wells
1979 ◽  
Vol 1979 (1) ◽  
pp. 287-291 ◽  
Author(s):  
Lawrence D. Neuman

ABSTRACT On the initiative of the States of the Region, in response to their large-scale development activities and the threat posed to the marine environment, the Kuwait Regional Conference of Plenipotentiaries on the Protection and Development of the Marine Environment and the Coastal Areas was convened by the Executive Director of the United Nations Environment Programme (UNEP) in Kuwait from 15–23 April 1978. The Conference was attended by Bahrain, Iran, Iraq, Kuwait, Oman, Qatar, Saudi Arabia and the United Arab Emirates. The major achievement of the Conference was the adoption of a Final Act which includes an Action Plan containing environmental assessment and management programs as well as the Kuwait Regional Convention for Co-operation in the Protection of the Marine Environment from Pollution and a Protocol concerning Regional Co-operation in Combating Pollution by Oil and other Harmful Substances in Cases of Emergency. The potential for severe environmental degradation from massive oil spills was recognized as the priority concern. Initial project activities are scheduled to begin in early 1979 and continue for two years. UNEP will act as the catalytic agent in what is a co-ordinated effort of the United Nations system. In addition to an assessment of the origin and magnitude of pollution in the Region, the unprecedented growth of coastal development, especially industry, will be assessed in order to evaluate environmental consequences and appropriate pollution control measures.


2005 ◽  
Vol 33 (2) ◽  
pp. 240-255 ◽  
Author(s):  
Heiki Lindpere

Article 292 of the United Nations 1982 Convention on the Law of the Sea (Convention) reads:1. Where the authorities of a state party have detained a vessel flying the flag of another state party and it is alleged that the detaining state has not complied with the provisions of this Convention for the prompt release of the vessel or its crew upon posting of a reasonable bond or other financial security, the question of release from detention may be submitted to any court or tribunal agreed upon by the parties or, failing such agreement within 10 days from the time of detention, to a court or tribunal accepted by the detaining state under article 287 or to the International Tribunal for the Law of the Sea, unless the parties otherwise agree.2. The application for release may be made only by or on behalf of the flag state of the vessel.3. The court or tribunal shall deal without delay with the application for release and shall deal only with the question of release, without prejudice to the merits of any case before the appropriate domestic forum against the vessel, its owner or its crew. The authorities of the detaining state remain competent to release the vessel or its crew at any time.4. Upon the posting of the bond or other financial security determined by the court or tribunal, the authorities of the detaining state shall comply promptly with the decision of the court or tribunal concerning the release of the vessel or its crew.


Author(s):  
Talitha Ramphal

Abstract Activities to tackle marine debris are conducted on the high seas by The Ocean Cleanup. The high seas are open to all States and may be used as long this is consistent with the United Nations Convention on the Law of the Sea (LOSC) and other rules of international law. This article argues that the LOSC provides for the freedom to use the high seas to protect and preserve the marine environment, including tackling marine debris, when interpreting Article 87 of the LOSC in light of present day needs.


2010 ◽  
Vol 10 (16) ◽  
pp. 7875-7890 ◽  
Author(s):  
B. R. Miller ◽  
M. Rigby ◽  
L. J. M. Kuijpers ◽  
P. B. Krummel ◽  
L. P. Steele ◽  
...  

Abstract. HFC-23 (also known as CHF3, fluoroform or trifluoromethane) is a potent greenhouse gas (GHG), with a global warming potential (GWP) of 14 800 for a 100-year time horizon. It is an unavoidable by-product of HCFC-22 (CHClF2, chlorodifluoromethane) production. HCFC-22, an ozone depleting substance (ODS), is used extensively in commercial refrigeration and air conditioning, in the extruded polystyrene (XPS) foam industries (dispersive applications) and also as a feedstock in fluoropolymer manufacture (a non-dispersive use). Aside from small markets in specialty uses, HFC-23 has historically been considered a waste gas that was, and often still is, simply vented to the atmosphere. Efforts have been made in the past two decades to reduce HFC-23 emissions, including destruction (incineration) in facilities in developing countries under the United Nations Framework Convention on Climate Change's (UNFCCC) Clean Development Mechanism (CDM), and by process optimization and/or voluntary incineration by most producers in developed countries. We present observations of lower-tropospheric mole fractions of HFC-23 measured by "Medusa" GC/MSD instruments from ambient air sampled in situ at the Advanced Global Atmospheric Gases Experiment (AGAGE) network of five remote sites (2007–2009) and in Cape Grim air archive (CGAA) samples (1978–2009) from Tasmania, Australia. These observations are used with the AGAGE 2-D atmospheric 12-box model and an inverse method to produce model mole fractions and a "top-down" HFC-23 emission history. The model 2009 annual mean global lower-tropospheric background abundance is 22.6 (±0.2) pmol mol−1. The derived HFC-23 emissions show a "plateau" during 1997–2003, followed by a rapid ~50% increase to a peak of 15.0 (+1.3/−1.2) Gg/yr in 2006. Following this peak, emissions of HFC-23 declined rapidly to 8.6 (+0.9/−1.0) Gg/yr in 2009, the lowest annual emission of the past 15 years. We derive a 1990–2008 "bottom-up" HFC-23 emission history using data from the United Nations Environment Programme and the UNFCCC. Comparison with the top-down HFC-23 emission history shows agreement within the stated uncertainties. In the 1990s, HFC-23 emissions from developed countries dominated all other sources, then began to decline and eventually became fairly constant during 2003–2008. By this point, with developed countries' emissions essentially at a plateau, the major factor controlling the annual dynamics of global HFC-23 emissions became the historical rise of developing countries' HCFC-22 dispersive use production, which peaked in 2007. Thereafter in 2007–2009, incineration through CDM projects became a larger factor, reducing global HFC-23 emissions despite rapidly rising HCFC-22 feedstock production in developing countries.


2010 ◽  
Vol 10 (5) ◽  
pp. 13179-13217
Author(s):  
B. R. Miller ◽  
M. Rigby ◽  
L. J. M. Kuijpers ◽  
P. B. Krummel ◽  
L. P. Steele ◽  
...  

Abstract. HFC-23 (also known as CHF3, fluoroform or trifluoromethane) is a potent greenhouse gas (GHG), with a global warming potential (GWP) of 14 800 for a 100-year time horizon. It is an unavoidable by-product of HCFC-22 (CHClF2, chlorodifluoromethane) production. HCFC-22, an ozone depleting substance (ODS), is used extensively in commercial refrigeration and air conditioning, in the extruded polystyrene (XPS) foam industries (dispersive applications) and also as a feedstock in fluoropolymer manufacture (a non-dispersive use). Aside from small markets in specialty uses, HFC-23 has historically been considered a waste gas that was, and often still is, simply vented to the atmosphere. Efforts have been made in the past two decades to reduce HFC-23 emissions, including destruction (incineration) in facilities in developing countries under the United Nations Framework Convention on Climate Change's (UNFCCC) Clean Development Mechanism (CDM), and by process optimization and/or voluntary incineration by most producers in developed countries. We present observations of lower-tropospheric mole fractions of HFC-23 measured by "Medusa" GC/MSD instruments from ambient air sampled in situ at the Advanced Global Atmospheric Gases Experiment (AGAGE) network of five remote sites and in Cape Grim air archive (CGAA) samples (1978–2009) from Tasmania, Australia. These observations are used with the AGAGE 2-D atmospheric 12-box model and an inverse method to produce model mole fractions and a "top-down" HFC-23 emission history. The model 2009 annual mean global lower-tropospheric background abundance is 22.8 (±0.2) pmol mol−1. The derived HFC-23 emissions show a "plateau" during 1997–2003, followed by a rapid ~50% increase to a peak of 15.0 (+1.3/−1.2) Gg/yr in 2006. Following this peak, emissions of HFC-23 declined rapidly to 8.6 (+0.9/−1.0) Gg/yr in 2009, the lowest annual emission of the past 15 years. We derive a 1990–2008 "bottom-up" HFC-23 emission history using data from the United Nations Environment Programme and the UNFCCC. Comparison with the top-down HFC-23 emission history shows agreement within the stated uncertainties. In the 1990s, HFC-23 emissions from developed countries dominated all other sources, then began to decline and eventually became fairly constant during 2003–2008. From the beginning of that plateau, the major factor determining the annual dynamics of global HFC-23 emissions became the historical rise of HCFC-22 production for dispersive uses in developing countries to a peak in 2007. Thereafter in 2007–2009, incineration through CDM projects became a larger factor, reducing global HFC-23 emissions despite rapidly rising HCFC-22 feedstock production in developing countries.


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