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| sector:other_and_natural_sources:natural_sources [2023/03/03 10:12] – [Table] hausmann | sector:other_and_natural_sources:natural_sources [2024/11/06 14:56] (current) – external edit 127.0.0.1 | ||
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| - | ====== | + | ====== 11 - Natural Sources ====== |
| - | ===== 11.C Other Natural Sources ===== | + | |
| - | ====Short description | + | |
| - | ^ NFR-Code | + | Within |
| - | | 11.C | + | |
| + | ^ NFR-Code | ||
| + | | 11.A | Volcanoes | ||
| + | | 11.B | [[sector: | ||
| + | | 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 NOx in the atmosphere. | ||
| - | ====Methodology==== | ||
| - | |||
| - | The calculation of NOx emissions from lightning uses strike counts from the German weather service and default emission factors from the EMEP/EEA guidebook. | ||
| - | |||
| - | 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 2 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 NOx from lightning is qualified estimated by expert judgement to be high (>50%). | ||
| - | |||
| - | ====Quality checks==== | ||
| - | No sector-specific quality checks are done. | ||
| - | |||
| - | ====Planned Improvement==== | ||
| - | Currently no improvements are planned. | ||