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Atmospheric Science for Environmental Scientists (eBook)

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2019 | 2. Auflage
John Wiley & Sons (Verlag)
978-1-119-51527-2 (ISBN)

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Enlightens readers on the realities of global atmospheric change, including global warming and poor air quality

Climate change and air pollution are two of the most pressing issues facing Mankind. This book gives undergraduate and graduate students, researchers and professionals working in the science and policy of pollution, climate change and air quality a broad and up-to-date account of the processes that occur in the atmosphere, how these are changing as Man's relentless use of natural resources continues, and what effects these changes are having on the Earth's climate and the quality of the air we breathe.

Written by an international team of experts, Atmospheric Science for Environmental Scientists, 2nd Edition provides an excellent overview of our current understanding of the state of the Earth's atmosphere and how it is changing. The first half of the book covers: the climate of the Earth; chemical evolution of the atmosphere; atmospheric energy and the structure of the atmosphere; biogeochemical cycles; and tropospheric chemistry and air pollution. The second half looks at cloud formation and chemistry; particulate matter in the atmosphere; stratospheric chemistry and ozone depletion; boundary layer meteorology and atmospheric dispersion; urban air pollution; and global warming and climate change science.

  • Provides succinct but detailed information on all the important aspects of atmospheric science for students
  • Offers the most up-to-date treatment of key issues such as stratospheric chemistry, urban air pollution, and climate change
  • Each chapter includes basic concepts, end-of-section questions, and more in-depth material
  • Features contributions from the best experts and educators in the field of atmospheric science

Atmospheric Science for Environmental Scientists, 2nd Edition is an invaluable resource for students, teachers, and professionals involved in environmental science. It will also appeal to those interested in learning how the atmosphere works, how humankind is changing its composition, and what effects these changes are leading to.



NICK HEWITT, PHD, is Distinguished Professor of Atmospheric Chemistry at Lancaster University, UK. His main research interests are in understanding how the biosphere and the atmosphere interact, how emissions of trace gases from the surface affect the composition and chemistry of the atmosphere, and how the changing atmospheric environment affects the world we live in.

ANDREA V. JACKSON, PHD, recently retired as Professor of Student Education and Engagement at the University of Leeds, UK. As well as conducting research in atmospheric chemistry, she worked with the UK's National Centre for Atmospheric Science on the development of their education and training programmes.

NICK HEWITT, PHD, is Distinguished Professor of Atmospheric Chemistry at Lancaster University, UK. His main research interests are in understanding how the biosphere and the atmosphere interact, how emissions of trace gases from the surface affect the composition and chemistry of the atmosphere, and how the changing atmospheric environment affects the world we live in. ANDREA V. JACKSON, PHD, recently retired as Professor of Student Education and Engagement at the University of Leeds, UK. As well as conducting research in atmospheric chemistry, she worked with the UK's National Centre for Atmospheric Science on the development of their education and training programmes.

Abbreviations, Constants, and Nomenclature


ADMS
Atmospheric Dispersion Modelling System
CEE
Central and eastern Europe
CCN
cloud condensation nuclei
CFC
chlorofluorocarbons
CO2
carbon dioxide
DMS
dimethyl sulphide
DNA
deoxyribonucleic acid
EC
elemental carbon
EM
electromagnetic
ENSO
El Niño–Southern Oscillation
EPA
Environmental Protection Agency
EU
European Union
GDP
global domestic product
GEMS/AIR
Global Environmental Monitoring System/Air
GHG
greenhouse gas
HAP
hazardous air pollutant
HCFC
hydrochlorofluorocarbons
HFC
hydrofluorocarbons
IAM
integrated assessment models
IBL
internal boundary layer
IPCC
Intergovernmental Panel on Climate Change
IR
infrared
ISAM
integrated science assessment model
ITCZ
intertropical convergence zone
LAI
leaf‐area index
LW
longwave
NMHC
non‐methane hydrocarbons
MAP
major air pollutant
MTBE
methyl‐tert‐butyl ether
NDVI
normalized difference vegetation index
OCS
carbonyl sulphide
OECD
Organization for Economic Cooperation and Development
PAH
polycyclic aromatic hydrocarbons
PAN
peroxyacetyl nitrate
PAR
photosynthetically active radiation
PCB
polychlorinated biphenyls
PFC
perfluorogenated carbon
PM
particulate matter
PM10
particles with aerodynamic diameter less than 10 μm
ppm
parts per million
ppmv
part per million by volume (1 × 10−6)
ppbv
part per billion by volume (1 × 10−9)
pptv
part per trillion by volume (1 × 10−12)
PSS
photostationary state
SAFARI
South African Regional Science Initiative
SW
shortwave
TSP
total suspended particulates
UNEP
United Nations Environmental Programme
UV
ultraviolet
VSLS
very short‐lived substances
VOC
volatile organic compounds
WHO
World Health Organization
WMO
World Meteorological Organization

Constants


c
speed of light in vacuum 2.998 × 108 m s−1
g
acceleration due to gravity 9.8 m s−2
h
Planck’s constant 6.626 × 1034 J s
k
Boltzmann constant 1.381 × 1034 J K−1
R
gas constant 8.314 J K−1 mol−1 (1.3 × 105 l atm mol−1 K−1)
Γd
dry adiabatic lapse rate 9.81 K km−1
π
3.14159
σ
Stefan–Boltzmann constant 5.67 × 10−8 W m−2 K−4

Nomenclature


a
radius of a particle
A
albedo
A s
surface albedo
B
radiative intensity of a blackbody
c p
specific heat capacity of dry air at constant pressure (1004 J kg−1 K−1)
c v
specific heat at constant volume
C
concentration (ppm or kg m−3)
d
preface to variable indicating incremental quantity
d
displacement height (m)
dQ
incremental change in heat
du
incremental change in internal energy
dv
incremental change in volume
dw
incremental change in work
e
turbulent kinetic energy per unit mass (J kg−1)
F B
the total flux from a black body radiator
F s
incoming solar radiation absorbed at the surface
F
net flux
F
upwelling radiative flux
F
downwelling radiative flux
net flux leaving an element or layer
F r
total upward reflected shortwave flux
F 0
incident solar flux
G
ground heat flux (W m−2)
h
mean height of roughness elements (m)
h b
depth of internal boundary layer (m)
H
sensible heat flux (W m−2) or mean building height (m)
H s
scale height
H/W
aspect ratio (‐)
I
intensity of light
I 0
initial intensity of light
k
von Kármán’s constant ≈ 0.4 (‐)
k a
absorption coefficient
k e
extinction coefficient
k s
scattering coefficient
l
distance through a gas interacting with light
L
latent heat of vaporization
L
Obukhov length (m)
L w
Liquid water content
L x
integral (or decorrelation) lengthscale (m)
m
refractive index
M
molar mass (of air unless otherwise specified)
n
number concentration, typically of absorbers or scatterers
p(u)
probability of windspeed u (‐)
P
plant area index (‐)
P, p
pressure
q
specific humidity (kg kg−1, sometimes g kg−1) or source emission rate (kg s−1)
q *
scaling parameter for specific humidity profile (kg kg−1, sometimes g kg−1)
r
radial distance
r v
mass mixing ratio of water vapour
r w
saturation mixing ratio
r r
scattered fraction reflected upwards
R
radius of the Earth
R(λ)
action spectrum
R n
net radiation (W m−2)
S
Solar constant
Sk u
skewness statistic for downstream component of the wind (‐)
Sk w
skewness statistic for vertical component of the wind (‐)
t
time (s)
t r
scattered fraction transmitted downwards
t t
total fraction of radiation transmitted downwards
T
temperature
T a
transmittance of the atmosphere
T e
effective blackbody temperature of the Earth
T L
integral timescale (s)
T *
scaling parameter for temperature profile (°C)
u
downstream velocity component (m s−1)
mean component (m s−1)
u
fluctuation around mean component (m s−1)
u *
friction velocity (m s−1)
U
velocity vector (m s−1)
(z)
vertical mean wind profile (m s−1)
mean windspeed at the top of a canopy (m s−1)
v
lateral velocity component (m s−1)
w
vertical velocity component (m s−1)
W
along wind building spacing (m)
x
horizontal distance in downstream direction (m)
y
horizontal distance in lateral direction (m)
z
distance, usually altitude (m)
z h
roughness length for heat transfer (m)
z m
height of maximum plant area index (m)
z 0
roughness length for momentum transfer (m)
z 0r
roughness length for rural surface (m)
z 0u
roughness length for urban surface (m)
z q
roughness length for moisture transfer (m)
z*
roughness sublayer depth (m)
z/L
Monin‐Obukhov stability parameter (‐)
σ
standard deviation (depends on quantity)
σ x
downstream plume spread (m)
σ y
lateral plume spread (m)
σ z
vertical plume spread (m)
σ(λ)
absorption cross section as a function of wavelength
β
upscatter or backscatter fraction
γ s
saturated adiabatic lapse rate
∆S
storage term (W m−2)
∆T
temperature difference between rural and...

Erscheint lt. Verlag 13.12.2019
Sprache englisch
Themenwelt Naturwissenschaften Biologie Ökologie / Naturschutz
Naturwissenschaften Geowissenschaften Geologie
Naturwissenschaften Geowissenschaften Meteorologie / Klimatologie
Technik Umwelttechnik / Biotechnologie
Schlagworte air quality • Atmosphere • atmospheric chemistry • Atmospheric Physics & Chemistry • atmospheric science biogeochemical • atmospheric sciences • biosphere • boundary layer</p> • climate change • earth sciences • environmental • Environmental Science • Environmental Studies • Geowissenschaften • global atmospheric change • global warming • Klimatologie u. Meteorologie • <p>environment • meteorology • Ozone • Physik u. Chemie der Atmosphäre • pollution • Umweltforschung • Umweltwissenschaften
ISBN-10 1-119-51527-0 / 1119515270
ISBN-13 978-1-119-51527-2 / 9781119515272
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