meta data for this page
Differences
This shows you the differences between two versions of the page.
Both sides previous revisionPrevious revisionNext revision | Previous revision | ||
sector:other_and_natural_sources:natural_sources [2023/04/13 09:22] – [Table] kotzulla | sector:other_and_natural_sources:natural_sources [2024/11/06 14:56] (current) – external edit 127.0.0.1 | ||
---|---|---|---|
Line 1: | Line 1: | ||
- | ===== 11.C - Other Natural Sources ===== | + | ====== 11 - Natural Sources |
- | ====Short description ==== | + | Within **11 - Natural Sources**, natural activities and resulting emissions are considered. |
- | ^ NFR-Code | + | ^ NFR-Code |
- | | 11.C | + | | 11.A | Volcanoes |
+ | | | ||
+ | | 11.C | [[sector: | ||
- | Lightning and corona discharge during thunderstorm events cause atmospheric chemical reactions to take place at high voltages and high temperatures. These reactions cause the production of NO< | ||
- | |||
- | ====Methodology==== | ||
- | |||
- | The calculation of NO< | ||
- | |||
- | For the complete time series, the emissions are calculated as follows: | ||
- | |||
- | <WRAP center round info 50%> | ||
- | **EM** = **AD** (number of lightning strikes) * ** EF** (kg emission per strike) | ||
- | </ | ||
- | |||
- | ===Activity data === | ||
- | The number of lightning strikes in Germany is taken from a commercial system called " | ||
- | |||
- | Table 1: Lightning strikes in Germany from 1990 onwards | ||
- | ^ Year ^ Strike count [1000 strikes] | ||
- | | 1990 | 443 | | ||
- | | 1991 | 443 | | ||
- | | 1992 | 370 | | ||
- | | 1993 | 274 | | ||
- | | 1994 | 429 | | ||
- | | 1995 | 394 | | ||
- | | 1996 | 218 | | ||
- | | 1997 | 255 | | ||
- | | 1998 | 428 | | ||
- | | 1999 | 589 | | ||
- | | 2000 | 1,026 | | ||
- | | 2001 | 591 | | ||
- | | 2002 | 1,023 | | ||
- | | 2003 | 813 | | ||
- | | 2004 | 741 | | ||
- | | 2005 | 802 | | ||
- | | 2006 | 1,001 | | ||
- | | 2007 | 1,139 | | ||
- | | 2008 | 990 | | ||
- | | 2009 | 917 | | ||
- | | 2010 | 589 | | ||
- | | 2011 | 687 | | ||
- | | 2012 | 656 | | ||
- | | 2013 | 542 | | ||
- | | 2014 | 623 | | ||
- | | 2015 | 550 | | ||
- | | 2016 | 432 | | ||
- | | 2017 | 443 | | ||
- | | 2018 | 446 | | ||
- | | 2019 | 329 | | ||
- | | 2020 | 399 | | ||
- | | 2021 | 512 | | ||
- | |||
- | ===Emission factor=== | ||
- | For the calculation of emissions in this category, the Guidebook emission factor of 2.75 kg NOx per strike is used. | ||
- | |||
- | ====Emission Trend==== | ||
- | The emission value is solely dependent on the strike count and varies between 1 to 3 kilotons of NOx per year. | ||
- | |||
- | Figure 1: NFR 11.C, NOx emissions from lightning | ||
- | |||
- | {{ : | ||
- | |||
- | ===== Recalculations ===== | ||
- | |||
- | <WRAP center round info 60%> | ||
- | As these activities and emissions are reported for the first time, no specific recalculations occur against a previous submission. | ||
- | </ | ||
- | |||
- | |||
- | ==== Uncertainties ==== | ||
- | The AD from BLIDS does have a low uncertainty of ± 3%. The uncertainties for the emission factors are estimated to be relatively high, being a default value. Hence the overall uncertainty for the emission estimation of NO< | ||
- | |||
- | ====Quality checks==== | ||
- | No sector-specific quality checks are done. | ||
- | |||
- | ====Planned Improvement==== | ||
- | Currently no improvements are planned. | ||