Hi All

If my decrypting of the Met. Speak encoding is correct this sounds quite 
encouraging.  The 50% increase in nuclei concentration under clouds is quite a 
modest dose. Working at latitudes between 30N and 30S at the same spray with 
the full dispersion width of the accumulation mode of aerosol sizes is so 
boring.  It would interesting to know what the concentrations were before 
treatment so that we could calculate the amount spray and the number of spray 
vessels needed.

If the concentrations were like the ones given by Vallina in 
doi:10.1029/2006GB002787 and the spray was monodisperse with a liquid diameter 
of 0.8 microns so as to avoid wasting energy on spraying salt mass very much 
heavier than Kohler would recommend,  we would need about a hundred vessels 
spraying  15 kg of water per second.

They will not all be working at full power and not all in the right place at 
the right time but some of this would be offset by an even more sophisticated 
planning of vessel movements based on real-time satellite observations and 
clever climate planners with ginormous quantum computers.  I predict that they 
would find the temperature gradients across oceans a very useful guide.

Stephen

Emeritus Professor of Engineering Design
School of Engineering
Mayfield Road  EH9 3 DW
University of Edinburgh
Scotland.
Tel 0131 662 1180

From: [email protected] <[email protected]> On 
Behalf Of Andrew Lockley
Sent: 09 February 2021 15:27
To: geoengineering <[email protected]>
Subject: [geo] Extreme climate response to marine cloud brightening in the arid 
Sahara-Sahel-Arabian Peninsula zone

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Extreme climate response to
marine cloud brightening in the
arid Sahara-Sahel-Arabian
Peninsula zone
Yuanzhuo Zhu
Climate Modeling Laboratory, School of Mathematics, Shandong University,
Jinan, China
Zhihua Zhang
Climate Modeling Laboratory, School of Mathematics, Shandong University,
Jinan, China and MOE Key Laboratory of Environmental Change and Natural
Disaster, Beijing Normal University, China, and
M. James C. Crabbe
Wolfson College, Oxford University, Oxford, UK; Institute of Biomedical and
Environmental Science and Technology, University of Bedfordshire, Luton, UK
and School of Life Sciences, Shanxi University, Taiyuan, China
Abstract
Purpose – Climatic extreme events are predicted to occur more frequently and 
intensely and will significantly
threat the living of residents in arid and semi-arid regions. Therefore, this 
study aims to assess climatic extremes’
response to the emerging climate change mitigation strategy using a marine 
cloud brightening (MCB) scheme.
Design/methodology/approach – Based on Hadley Centre Global Environmental Model 
version 2-
Earth System model simulations of a MCB scheme, this study used six climatic 
extreme indices [i.e. the hottest
days (TXx), the coolest nights (TNn), the warm spell duration (WSDI), the cold 
spell duration (CSDI), the
consecutive dry days (CDD) and wettest consecutive five days (RX5day)] to 
analyze spatiotemporal evolution
of climate extreme events in the arid Sahara-Sahel-Arabian Peninsula Zone with 
and without MCB
implementation.
Findings – Compared with a Representative Concentration Pathways 4.5 scenario, 
from 2030 to 2059,
implementation of MCB is predicted to decrease the mean annual TXx and TNn 
indices by 0.4–1.7 and 0.3–
2.1°C, respectively, for most of the Sahara-Sahel-Arabian Peninsula zone. It 
would also shorten the mean
annual WSDI index by 118–183 days and the mean annual CSDI index by only 1–3 
days, especially in the
southern Sahara-Sahel-Arabian Peninsula zone. In terms of extreme 
precipitation, MCB could also decrease
the mean annual CDD index by 5–25 days in the whole Sahara and Sahel belt and 
increase the mean annual
RX5day index by approximately 10 mm in the east part of the Sahel belt during 
2030–2059.
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