Airborne fraction

Feccere airborne ko faktoriyaal scaling sifotoongal ko njuuteendi ɓeydagol hitaande kala e nder weeyo CO

2 haa CO

2 ɓuuɓri ummoraade e iwdiiji aadee.Ina hollita keewal CO2 neɗɗo yaltuɗo e weeyo. Teskagol e nder duuɓi capanɗe jeegom jawtuɗi ɗii ina hollita wonde feccere weeyo ina heddii e 45%. Ɗum hollitii wonde leydi ndii e geec ina mbaawi mooftude CO2 ina jokki e ɓeydagol CO2 neɗɗo, hay so tawii noon ko feere teeŋtunde e nder leydi e nder leydi, tawa noon ko ɓuri heewde e mum en ina addana leydi ndii waawde huutoraade CO2. Won ko holliti ɓeydagol ko ɓooyaani e feccere weeyo, ɗum firti ko ɓeydagol ɓurngol yaawde e CO weeyo

2 ngam limgal limgal fossil-fuel neɗɗo. Waylooji e nder sinkiiji karbon ina mbaawi battinde e feccere weeyo kadi.CO2 antropojenik yaltuɗo e weeyo ina feccii e geɗe tati : ko ina tolnoo e 45% ina heddii e weeyo (ina wiyee ko feccere weeyo), tawi noon ko ina wona 24% e 31% ina moofta ɗum e geec (sayfeer ocean) e biosfeer leydi (says leydi). So tawii feccere weeyo ndee ɓeydiima, ɗum ina hollita wonde CO2 mo aadee yaltinta oo, ina soomi e leydi e ƴiye geec, sabu geɗe bayɗe no geec ɓuuɓɗo walla permafrost ɓuuɓɗo. Ko ɗum waɗi, ko ɓuri heewde e mborosaaji anthropogenic ina keddii e weeyo, ɗum noon ina yaawi tolno mbayliigu weeyo. Ɗuum ina jogii batte e ƴeewndooji garooji to bannge toɓɓe CO2 weeyo, ɗe poti ko ƴeewteede ngam hiisaade ngool laawol.Naamnal so tawii feccere weeyo ina ɓeydoo, heddii ko ina heddii e ko ina tolnoo e 45%, walla ustaare ina heddii e haala. Resndo ndee naamndal ina teskaa sabu faamde cirƴam karbon adunaare ndee, ina jogii nafoore wonande waɗooɓe politik e renndo ngoo fof.{\hollirde AF_{FF}={\frac {\frac {dC(t)}{dt}}{FF(t)}}}

Mala,

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{\hollirde AF_{FF+LU}={\frac {\frac {dC(t)}{dt}}{FF(t)+LU(t)}}}

E nder ɗuum C woni gaas karbonik weeyo, t woni waktu, FF woni ɓuuɓol fossil-fuel e LU woni ɓuuɓol feewde e weeyo sabu waylo-waylo kuutoragol leydi.

E jooni jooni, wiztooji vurzi yuurnitaade yah-ngartaa e feccere weeyo ina peeñnina batte luurondirɗe, tawi noon vursugol ngol ina jokkondiri e kuutoragol leydi e mbayliigu vursugol leydi ina hollira vursugol ɓurngol maantinde e ŋakkeende hoolaare. Won e wiɗtooji kollitii wonde alaa ko holliti limtooji kollitooji ɓeydagol feccere weeyo e feccere weeyo hiisaande hono,

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{\hollirde AF={\frac {G_{t}}{E_{FF}+E_{LUC}}}}

Ɗo Gt woni mawnugol CO2 weeyo, EFF woni ɓuuɓol ɓuuɓol fossil-fuel, ELUC woni ɓuuɓol mbayliigu kuutoragol leydi.

Hujja goɗɗo hollitaama wonde feccere CO2 nde golle aadee yaltinta e nder weeyo, haa teeŋti noon e mbayliigu nguura, peewnugol semmbe, e waylooji kuutoragol leydi, ina ɓeydoo. Gila hitaande 1959, CO2 gonɗo e weeyo ko 0,43, kono ina hollita ɓeydagol ko ina tolnoo e 0,2% e hitaande kala e nder oon sahaa.

</ref> Changes in carbon sinks can affect the airborne fraction as well.

 Discussion about the trend of airborne fraction 
Anthropogenic CO2

Annduɓe mbayliigaaji feccere weeyo ina mbaawi battinde e geɗe tawaaɗe e yaasi, ko wayi no El Niño-Oscillation (ENSO), ɓuuɓol kaaƴe, e geɗe goɗɗe nannduɗe heen.[8] Ina gasa tawa laabi kuutorteeɗi e ɗeen wiɗtooji ngam yuurnitaade mbaydi feccere weeyo ngo ngonaa tiiɗɗi, ɗum noon, ciimtol ngol ƴettaa e majji ngol alaa ko foti.</ref> This indicates that the land and ocean's capacity to absorb CO2 has kept up with the rise in human CO2 emissions, despite the occurrence of notable interannual and sub-decadal variability, which is predominantly driven by the land's ability to absorb CO2

Ƴeew kadi

Gaasuuji ɓuuɓɗi

Gaas karbonik e nder weeyo Leydi

Reso ƴeewndo Kolonel Karbon Total

Tagoore karbon weeyo

 Tuugnorgal 
Keewgol “feccere henndu” ndee, ko Charles David Keeling inniti ɗum e hitaande 1973, e wiɗtooji baɗaaɗi e kitaale 1970 e kitaale 1980 cifaaɗi feccere airborne ummoraade e mbayliigu limto karbon ka, hono,

Yeewtere e mbaydi feccere aeroport