Energy Indicators for Sustainable Development: Guidelines and Methodologies International Atomic Energy Agency United Nations Department of Economic and Social Affairs International Energy Agency Eurostat European Environment Agency


(c) International Conventions and Agreements



Yüklə 0,94 Mb.
Pdf görüntüsü
səhifə93/159
tarix30.04.2023
ölçüsü0,94 Mb.
#105269
1   ...   89   90   91   92   93   94   95   96   ...   159
pub1222 web

(c) International Conventions and Agreements: The United Nations Framework 
Convention on Climate Change (UNFCCC) entered into force in March 1994. The 
Convention included a commitment by Parties, both developed countries and 
economies in transition (Annex I Parties), to aim to return emissions of CO
2
and other 
GHGs not controlled by the Montreal Protocol to their 1990 levels by 2000, although 
relatively few Parties actually met this goal. The Kyoto Protocol was adopted in 
December 1997. It was designed to enter into force after being ratified by at least 55 
Parties to the Convention, including developed countries accounting for at least 55% 
of the total 1990 CO
2
emissions from this group. With the 2004 decision by the 
Russian Federation to ratify the Protocol, it entered into force in early 2005. In any 
event, countries are also bound by their commitments under the Convention. 
Ozone-depleting GHGs are controlled by the Vienna Convention and the Montreal 
Protocol. 
(d) International Targets/Recommended Standards: The Kyoto Protocol sets 
targets for each Annex I Party with a view to reducing these Parties’ overall emissions 
of the six main GHGs by at least 5% below 1990 levels in the commitment period 
2008–2012. 
(e) Linkages to Other Indicators: This indicator is closely linked to many other 
economic and environmental indicators, including energy use per capita and per unit 
of GDP, primary and final energy use and electricity generation, fuel mix, 
atmospheric emissions, etc. 
METHODOLOGICAL DESCRIPTION 
(a) Underlying Definitions and Concepts: GHGs contribute in varying degrees to 
global warming depending on their heat absorption capacity and their lifetime in the 
atmosphere. The GWP describes the cumulative radiative forcing effect of a gas over 
a time horizon (usually chosen for reporting purposes to be 100 years) compared with 
that of CO
2
. For example, the 100-year GWP of CH
4
is 21, meaning that the global 
warming impact of 1 kilogram (kg) of CH
4
is 21 times higher than that of 1 kg of 
CO
2
. The GWP of N
2
O is 310. No GWPs are provided for indirect GHGs. Sinks for 
GHGs should not be included in the indicator. There are currently no agreed 
international inventory methodologies for the quantification of engineered sinks in 
which energy-related GHG emissions can potentially be captured and stored, while 
biological sinks are not directly linked with energy-related GHG emissions. 

Yüklə 0,94 Mb.

Dostları ilə paylaş:
1   ...   89   90   91   92   93   94   95   96   ...   159




Verilənlər bazası müəlliflik hüququ ilə müdafiə olunur ©azkurs.org 2024
rəhbərliyinə müraciət

gir | qeydiyyatdan keç
    Ana səhifə


yükləyin