https://link.springer.com/article/10.1007/s42452-021-04388-9?s=03#Ack1

Precipitation and temperature response to sea salt injection into low
marine clouds over West Africa
Mojisola O. Adeniyi & Blessing E. I. Bassey
SN Applied Sciences volume 3, Article number: 378 (2021) Cite this article

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Abstract
Sea salt injection into the tropical marine clouds is evaluated for its
potentials to reduce the negative impact of the prevailing global warming
over West Africa. Radiative forcing is determined as the intercept of the
regression of response of radiation parameter to that of surface air
temperature. The seasonal responses of temperature and precipitation to
geoengineering over West Africa are analysed using temperature and
precipitation outputs from IPSL-M5A-LR with three different forcing
scenarios. The three scenarios are historical greenhouse gas
concentrations, Representative Concentration Pathway 4.5 W/m2 scenario
(RCP4.5) and combination of RCP4.5 and geoengineering forcing (sea salt
climate engineering, G5). 20-year means in the middle of G5 (2045–2064) are
considered for the future period, and the historical climatology from 1986
to 2005 is used. Net downward flux and top of atmosphere outgoing shortwave
radiation have negative forcing only at the western Sahel. The G5 reduces
the warming in the RCP4.5 scenario over the whole of West Africa. It also
shifts ITCZ northward with respect to RCP4.5, thereby increasing wetness
over most of the land areas. The areas with wetness response have anomalous
westerly with respect to RCP 4.5 and latitudinal location below anomalous
easterly wind. Results show that G5 is effective in reducing the RCP4.5
projected warming up to 1.2 K and increasing wetness over most land areas.
The G5 has a damaging effect on the temperature pattern at the southern
ocean and coastal areas, while it has damaging effect on precipitation
patterns at some parts of the Sahel.

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