The direct radiative forcing due to non-methane hydrocarbons (NMHCs) has no
t previously been quantified. We use new measurements of infrared absorptio
n cross-sections and a narrow band radiative transfer model to estimate a f
orcing. An upper limit to the global mean anthropogenic forcing is likely t
o be in the region of 0.015 W m(-2), less than 1% of the forcing due to oth
er greenhouse gases. However, taking account of the natural NMHC loading an
d the vertical profile of these gases the actual radiative forcing is likel
y to be somewhat less than this. (C) 1999 Elsevier Science Ltd. All rights
reserved.