CH2O

Also, CH 2 O levels found in the marine boundary layer
(MBL) over the tropical Atlantic during the Transport and
Atmospheric Chemistry Near the Equator—Atlantic (TRACE-A)
campaign were much lower than predicted by model calculations
[Jacob et al., 1996; Heikes et al., 1996a]. As a possible reason
for the model overestimate by a factor of 3, the complexation of
CH 2 O with organics in the marine aerosol was speculated [Jacob
et al., 1996].
[ 5 ] On the other hand, Ayers et al. [1997] measured CH 2 O
concentrations around 300 pptv at Cape Grim (Tasmania), 50%
higher than predicted by their model. They point to the reaction
of CH 3 O 2 with HO 2 that in the standard reaction scheme yields
CH 3 O 2 H with 100% yield. Ayers et al. [1997] proposed a
second reaction channel directly producing CH 2 O and showed
that a 40% yield of this branch is sufficient to resolve the
discrepancy between model and measurement.
https://www.academia.edu/30457249/Are_CH2O_measurements_in_the_marine_boundary_layer_suitable_for_testing_the_current_understanding_of_CH4_photooxidation_A_model_study?email_work_card=view-paper

Carbon dioxide (CO2), nitrous oxide (N2O), and methane (CH4) are each important to climate forcing and to the levels of stratospheric ozone (see Chapter 2). In terms of the globally averaged ozone column, additional N2O leads to lower ozone levels, whereas additional CO2 and CH4 lead to higher ozone levels. Ozone depletion to date would have been greater if not for the historical increases in CO2 and CH4. The net impact on ozone recovery and future levels of stratospheric ozone thus depends on the future abundances of these gases. For many of the scenarios used in the most recent Intergovernmental Panel on Climate Change (IPCC) Assessment (IPCC, 2013), global ozone will increase to above pre-1980 levels due to future trends in the gases.
https://csl.noaa.gov/assessments/ozone/2014/summary/ch5.html

James_ wrote:
An increase or decrease in the speed of the wind changes its momentum. It's warmer when air slows. Also, verifying trigonometric identities can be used to consider how atmospheric gasses can allow for a change in the different levels of certain atmospheric gasses. This is where sets and intersections/unions can help define what gasses allow for what other gasses to occur. The verifying trigonometric identities will help to support such changes in atmospheric gasses.