Biomass Burning Kills 250,000 People a Year

-  by Jo Nova, August 5, 2014, JoanneNova.com.au

The head­line at Sci­ence Dai­ly is that wild­fires and oth­er burns lead to cli­mate change. The paper itself asks: “As such, par­ti­cle burn-off of clouds may be a major under­rec­og­nized source of glob­al warm­ing.” For me what mat­ters are the deaths in the here and now:

“We cal­cu­late that 5 to 10 per­cent of world­wide air pol­lu­tion mor­tal­i­ties are due to bio­mass burn­ing,” Jacob­son said. “That means that it caus­es the pre­ma­ture deaths of about 250,000 peo­ple each year.”

 This is sim­i­lar to Indur Goklany’s con­clu­sion in 2011:

Killing peo­ple with “con­cern”? Bio­fu­els led to near­ly 200,000 deaths (est) in 2010.

In a study  pub­lished in  Jour­nal of Amer­i­can Physi­cians and Sur­geons, Indur Gok­lany cal­cu­lat­ed the addi­tion­al mor­tal­i­ty bur­den of bio­fu­els poli­cies and found that near­ly 200,000 peo­ple died in 2010 alone, because of efforts to use bio­fu­els to reduce CO2 emissions.

Gok­lany (2011) esti­mat­ed that the increase in the pover­ty head­count due to high­er bio­fu­el pro­duc­tion between 2010 and 2004 implies 192,000 addi­tion­al deaths and 6.7 mil­lion addi­tion­al lost DALYs in 2010 alone.

He com­pared this death tal­ly to the WHO fig­ures for deaths attrib­uted to glob­al warm­ing and finds that the bio­fu­els poli­cies are more dead­ly. (And he is not includ­ing any increase in pover­ty due to oth­er anti-glob­al warm­ing practices).

What rather mat­ters is how much of this is “wild” fire and how much is agri­cul­tur­al fire. Indur Goklany’s work looked specif­i­cal­ly at bio­fu­els, so relat­ed to man-made air pol­lu­tion. From the actu­al Jacob­sen paper it’s clear that this is most­ly thought to be man-made fires:

Seil­er and Crutzen [1980] fur­ther esti­mat­ed that wild­fires in tem­po­ral plus bore­al forests com­prised ~35.7% of all dry mat­ter burned but point­ed out that 70–90% of such wild­fires were due to human activ­i­ty (e.g., camp­fires, debris burn­ing, cig­a­rettes, etc.). Thus, of total world fire emis­sions today, ~7.1% (3.6%–10.7%) may be nat­ur­al and the rest, anthro­pogenic. Houghton [2005] indi­cates that, in 1850, CO2 emis­sions from land use change may have been ~34% those in 2005. Thus, in 1850, BB [Burn­ing Bio­mass] emis­sions were low­er than those today. Such emis­sions may have been most­ly anthro­pogenic [e.g.,  Mar­lon et al., 2008] although part­ly nat­ur­al as well. Today, BB emis­sions are much high­er with only a small per­cent natural.

Does black car­bon change clouds?

The study goes on to say that black car­bon effec­tive­ly caus­es glob­al warm­ing too because it heats water droplets, melts clouds and ice,  and reduces the thick­ness of cloud cover.

So any minute now I expect envi­ron­men­tal­ists around the world will start a “Boy­cott Bio­mass” cam­paign. Clear­ly any tru­ly com­pas­sion­ate green could do noth­ing less since bio­mass is a net killer, and warms the plan­et too.

[Sci­ence Dai­ly] “But Jacobson’s research also demon­strates that it isn’t just the CO2 from bio­mass burn­ing that’s the prob­lem. Black car­bon and brown car­bon max­i­mize the ther­mal impacts of such fires. They essen­tial­ly allow bio­mass burn­ing to cause much more glob­al warm­ing per unit weight than oth­er human-asso­ci­at­ed car­bon sources.

Black and brown car­bon par­ti­cles increase atmos­pher­ic warm­ing in three ways. First, they enter the minus­cule water droplets that form clouds. At night, that’s not an issue. But dur­ing the day, sun­light scat­ters around with­in clouds, bathing them in luminescence.

When sun­light pen­e­trates a water droplet con­tain­ing black or brown car­bon par­ti­cles, Jacob­son said, the car­bon absorbs the light ener­gy, cre­at­ing heat and accel­er­at­ing evap­o­ra­tion of the droplet. Car­bon par­ti­cles float­ing around in the spaces between the droplets also absorb scat­tered sun­light, con­vert­ing it to heat.

“Heat­ing the cloud reduces the rel­a­tive humid­i­ty in the cloud,” Jacob­son said.

This caus­es the cloud to dis­si­pate. And because clouds reflect sun­light, cloud dis­si­pa­tion caus­es more sun­light to trans­fer to the ground and seas, ulti­mate­ly result­ing in warmer ground and air temperatures.

Final­ly, Jacob­son said, car­bon par­ti­cles released from burn­ing bio­mass set­tle on snow and ice, con­tribut­ing to fur­ther warming.

“Ice and snow are white, and reflect sun­light very effec­tive­ly,” Jacob­son said. “But because car­bon is dark it absorbs sun­light, caus­ing snow and ice to melt at accel­er­at­ed rates. That expos­es dark soil and dark seas. And again, because those sur­faces are dark, they absorb even more ther­mal ener­gy from the sun­light, estab­lish­ing an ongo­ing ampli­fi­ca­tion process.”

Jacob­son not­ed that some car­bon par­ti­cles — specif­i­cal­ly white and gray car­bon, the vari­ants asso­ci­at­ed with some types of ash — can exert a cool­ing effect because they reflect sun­light. That must be weighed against the warm­ing qual­i­ties of the black and brown car­bon par­ti­cles and CO2emis­sions gen­er­at­ed by bio­mass com­bus­tion to derive a net effect.

Jacob­son said the sum of warm­ing caused by all anthro­pogenic green­house gas­es — CO2, methane, nitrous oxide, chlo­ro­flu­o­ro­car­bons and some oth­ers — plus the warm­ing caused by black and brown car­bon will yield a plan­e­tary warm­ing effect of 2 degrees Cel­sius over the 20-year peri­od sim­u­lat­ed by the com­put­er. But light-col­ored par­ti­cles — white and gray par­ti­cles pri­mar­i­ly — reflect sun­light and enhance cloudi­ness, caus­ing more light to reflect.”

How much warm­ing does black car­bon cause?

Bio­mass burn­ing was cal­cu­lat­ed to cause 20 year glob­al warm­ing of ~0.4 K because CAE I (~32% of BB warm­ing), CAE II, semi­di­rect effects, AHFs (~7% of BB warm­ing), AMFs, and tar balls from bio­mass burn­ing togeth­er out­weighed indi­rect effects, con­trary to pre­vi­ous bio­mass burn­ing stud­ies that did not treat CAEs, AHFs, AMFs, or brown car­bon. AHFs from all sources and AMF + AHF from pow­er plants and elec­tric­i­ty use each account­ed for sta­tis­ti­cal­ly sig­nif­i­cant +0.03 K glob­al sur­face air tem­per­a­ture warming.

One-dimen­sion­al sim­u­la­tions helped to explain the strong effect on cloud burn-off of BB and BC from oth­er sources. They showed that when absorb­ing aerosols exist in clouds, instan­ta­neous direct radia­tive forc­ing (DRF) and sur­face tem­per­a­ture change are anti­cor­re­lat­ed because when absorb­ing aerosol burns off a cloud, the aerosol DRF decreas­es due to a decrease in opti­cal focus­ing, yet sur­face tem­per­a­ture esca­lates rapid­ly due to the pour­ing in of sun­light to the sur­face. As such, par­ti­cle burn-off of clouds may be a major under­rec­og­nized source of glob­al warm­ing.

REFERENCE

Mark Z. Jacob­son. Effects of bio­mass burn­ing on cli­mate, account­ing for heat and mois­ture flux­es, black and brown car­bon, and cloud absorp­tion effects.Jour­nal of Geo­phys­i­cal Research: Atmos­pheres, 2014; DOI: 10.1002/2014JD021861


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