k at the graph of radiative forcing. The strongest positive radiative forcing in the modern climate system comes |CFCS N,O CH, 2 Aerosols co, Black carbon from fossil fuels Tropospheric Solar Stratospheric Organic Biomass Land use Sulfate carbon burning Aerosol (albedo only) ozone from indirect effect fossil fuels High Medium Low Very low- Level of scientific understanding Sulfate Back carbon Land Use Solar variability Greenhouse gases Radiative forcing (W/m²)
k at the graph of radiative forcing. The strongest positive radiative forcing in the modern climate system comes |CFCS N,O CH, 2 Aerosols co, Black carbon from fossil fuels Tropospheric Solar Stratospheric Organic Biomass Land use Sulfate carbon burning Aerosol (albedo only) ozone from indirect effect fossil fuels High Medium Low Very low- Level of scientific understanding Sulfate Back carbon Land Use Solar variability Greenhouse gases Radiative forcing (W/m²)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question
![Look at the graph of radiative forcing. The strongest positive radiative forcing in the modern climate system comes from
CFCS
N,O
CH,
2
Aerosols
co,
Black
carbon
from
Tropospheric
fossil fuels
Solar
Stratospheric
ozone
Organic Biomass
carbon burning Aerosol (albedo
from
fossil fuels
Land use
Sulfate
indirect only)
effect
-2
High Medium
Low Very low-
Level of scientific understanding
Sulfate
Back carbon
Land Use
Solar variability
Greenhouse gases
Radiative forcing (W/m²)](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F52bb430e-739f-421e-b63f-b352d1f099d9%2Ff90e26c2-2126-4c46-a6cd-332805db0891%2F6ek5rh_processed.png&w=3840&q=75)
Transcribed Image Text:Look at the graph of radiative forcing. The strongest positive radiative forcing in the modern climate system comes from
CFCS
N,O
CH,
2
Aerosols
co,
Black
carbon
from
Tropospheric
fossil fuels
Solar
Stratospheric
ozone
Organic Biomass
carbon burning Aerosol (albedo
from
fossil fuels
Land use
Sulfate
indirect only)
effect
-2
High Medium
Low Very low-
Level of scientific understanding
Sulfate
Back carbon
Land Use
Solar variability
Greenhouse gases
Radiative forcing (W/m²)
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