Modeling of Atmospheric Chemistry

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Modeling of Atmospheric Chemistry Page 74

by Guy P Brasseur


  prior error, 496covariance matrix, 498

  variance, 491

  prior estimate, 487, 491, 494, 496

  prior information, 487

  prior PDF, 492

  probability density function, 489Gaussian PDFs for vectors, 501

  prognostic, 114

  proton transfer reaction mass spectrometer (PTR-MS), 439atmospheric components measured, 440–441

  PSCs. See ozone (O3), stratospheric: polar stratospheric clouds

  pseudo-density, 123

  PTR-MS. See proton transfer reaction mass spectrometer (PTR-MS)

  puff model, 170

  PVU. See potential vorticity unit

  pyroconvection, 408

  QBO. See quasi-biennial oscillation (QBO)

  quantum yield, 228

  quasi steady-state, 232

  quasi-biennial oscillation (QBO), 51

  quasi-geostrophic approximation, 110

  quasi-laminar boundary layer, 418

  radiance (intensity) definition, 206

  radiation definition, 205

  radiative source, 208

  radiative transfer definition, 205

  equation, 211–224source function, 250

  radiative transfer model, 12, 488, 513and remote sensing, 445

  radical-assisted reaction chains, 54

  radicals, 54

  RANS. See Reynolds averaged Navier–Stokes equation

  rate coefficient. See rate constant

  rate constant, 230

  rate-limiting step, 62

  Rayleigh scattering, 82, 217

  Rayleigh theory, 217

  reactive uptake probability, 242

  receptor-oriented problem, 502

  refraction index, 217

  regridding. See remapping

  regularization method, 490

  relative error variance reduction, 494

  relative humidity (RH), 29

  remapping, 184

  remote sensing, 487atmospheric components measured, 440–441

  differential optical absorption spectroscopy (DOAS), 445

  and Max-DOAS, 445

  Dobson spectrophotometers, 444

  filter radiometers, 445gas-filter correlation radiometry (GFCR), 446

  Fourier transform infrared (FTIR) spectroscopy, 446

  microwave spectroscopy, 447

  Umkehr effect, 444

  representation error, 491–492covariance matrix, 499

  vector, 498

  residual error method, 499–500

  retrieval, See optimal estimate

  residence lifetime. See e-folding lifetime

  resistance aerodynamic, 420

  quasi-laminar boundary resistance (boundary resistance), 421

  surface, 422

  total, to dry deposition, 420

  resistance-in-series model. See big-leaf model

  resonance fluorescence, 442atmospheric components measured, 440–441

  retrieval, of satellite observations aerosol optical depth (AOD), 460

  column concentrations, 459

  vertical profiles (optimal estimate), 459

  Reynolds decomposition, 343–349, 353

  Reynolds averaged Navier–Stokes equation, 107

  Reynolds number, 344–345

  Reynolds stress, 107

  RH. See relative humidity (RH)

  Richardson number, 345critical, 372

  riming, 384

  RMA. See linear regression

  RMSE. See root mean square error (RMSE)

  root mean square error (RMSE), See also centered root mean square error (CRMSE)

  roughness length, 375

  Rossby waves, 50

  RTM. See radiative transfer model

  saltation, 413

  SAO. See semi-annual oscillation (SAO)

  satellite measurements geostationary orbit, 453

  Lagrange L1 and L2 orbits, 453

  low Earth orbit (LEO), 453

  microwave instruments, 452

  Molniya orbit, 453

  solar backscatter instruments, 452

  thermal infrared (IR) instruments, 452

  saturation pressure, 29

  saturation vapor pressure. See saturation pressure

  scale height, 31

  scatterplots, See evaluation, model

  scattering of radiation, 217definition, 207

  scattering efficiency, 217, 219

  scattering phase function, 217

  scattering regimes diagram, 218

  Schmidt number, 421

  Schumann–Runge bands, 217, 228

  Schumann–Runge continuum, 217

  Schwarzschild’s equation, 224

  sea salt aerosol, 412

  sectional model, 96

  segregation ratio, 350

  semi-annual oscillation (SAO), 51

  semi-Lagrangian methods, 328–334

  semi-Lagrangian model, 328

  sensible heat, 23

  sequential updating, 516

  shallow atmosphere approximation, 103

  Shapiro filter, 179

  shape factor and satellite observations, 459

  shortwave radiation, 205. See also solar radiation

  Shuman filter, 179

  similarity assumption, 352

  similarity theory, 374

  single-scattering albedo, 81, 208

  slant optical depth, 207

  slant column and satellite observations, 459

  slip-correction factor, 427

  smog, 14

  smoothing, See filtering

  smoothing error, 494, 512covariance matrix, 512

  solar constant, 22, 213

  solar energy. See solar radiation

  solar radiation, 22absorption spectrum by O2 and O3, 215–231

  flux, 22–23

  and general circulation, 48–50

  and the global energy budget, 23

  in the mesosphere, 25

  and remote sensing, 444

  spectral density at top of the atmosphere, 213

  spectral irradiance at sea level, 213

  transfer of, in the atmosphere absorption and scattering, 217–218

  numerical solution, 222–223

  phase function, 220

  scattering by aerosols and cloud droplets, 218–219

  scattering by air molecules, 217

  source function, 220

  sondes. See ozonesondes

  specific humidity, 28

  spectral decomposition, 497, 501

  spectral density definition, 206

  formulation, 206

  spectral filter, 183response function, 183

  spectral methods fast Fourier transform (FFT), 152

  Fourier decomposition, 151

  Gaussian grid, 155

  Gibbs phenomenon, 153

  pseudo-spectral, 155

  rhomboidal truncation, 154

  spherical harmonics, 153

  triangular truncation, 154

  spectroscopy. See also remote sensingactive, 439

  passive, 439

  speed of light, 205

  s-stage, 138

  staggered grid, 143

  statistical model, 171

  stomata, of the leaf, 404, 422

  storm tracks, 44

  stability, 275amplification factor, 285–286, 288, 292, 360

  atmospheric, 345

  CFL. See CFL criterion

  conditional, 35

  convective, 366

  numerical, 285

  polar singularity, 336

  unconditional, 290

  unconditional instability, 285

  von Neumann analysis, 285–287

  standard gravity, 32

  state vector, 487, 496

  statistical metrics, of model skill correlation, 469, 471–473

  grading, 474

  other indices of agreement, 471

  outliers, 469

  statistical significance, 478–480

  Target diagram, 477

 
Taylor diagram, 475–477

  steepest-descent algorithm, 520

  Stefan–Boltzmann constant, 22, 211

  Stefan–Boltzmann law, 211

  steric factor, 230

  stiff system, 254

  STILT model, 370

  stochastic models, 4, 6, 8–9definition, 5

  of turbulence, 355

  Stokes–Einstein formula, 246

  stratiform precipitation. See large-scale precipitation

  stratopause, 25, 51

  stratosphere, 25, 27

  stratosphere–troposphere exchange, 25dynamical barriers, 351

  streamfunction, 111

  Student’s t-test, 473, 479, 586–588

  subsaturated, 29

  subsidence, 34, 378

  subsidence inversion in the free troposphere, 48

  successive order method, 222

  sulfur species, 74–75oxidation states, 75

  sulfur dioxide (SO2) aqueous-phase oxidation, 75

  gas-phase oxidation, 75

  supercomputer. See computing

  supercooled, 29

  supersaturated, 29

  surface layer, 367

  surface measurements. See observing platforms

  surface uptake. See dry deposition

  surrogate species, 234

  synoptic scale definition, 38

  systematic error. See mean bias

  tangent linear model, 507

  Target diagram. See statistical metrics, of model skill

  Taylor diagram. See Statistical metrics, of model skill

  Taylor expansion, 563

  TDL. See tunable-diode laser (TDL) spectroscopy

  temperature. See atmospheric temperature

  temperature inversion and atmospheric stability, 33

  definition, 25

  in the stratosphere, 25, 49

  in the troposphere, 34

  ternary nucleation, 245

  terminal settling velocity, 427

  terrestrial IR. See terrestrial radiation

  terrestrial radiation. See infrared (IR) radiation

  terrestrial radiation absorption by molecules, 225

  emission of, 224–225

  numerical solutions of transfer equation, 225–227

  spectrum, 205

  thermolysis, 229

  third body, 55, 231

  three-body reaction, 231–232broadening factor, 232

  high-pressure limit, 232

  low-pressure limit, 232

  reaction rate, 231

  Tikhonov regularization, 491, 527matrix, 527

  time smoothing Robert–Asselin, 184

  TLM. See tangent linear model

  top-down constraint, 488

  total derivative, 561definition, 561

  trajectory model, 160

  troposphere. See also free troposphere

  thermal wind, 40–41, 370

  thermal wind equations, 39application to the stratosphere, 49

  thermopause, 25

  thermosphere, 25–26

  thermosphere, 27

  third body, 231

  top-down constraint, 401

  trace gas definition, 21, 277

  trade winds, 42, 44and El Niño–Southern Oscillation, 47

  transfer velocity. See exchange velocity

  transition regime, 241

  transmission function, 207

  transportivity, 276, 289

  Troe expression, 232

  tropical pipe, 52, 390

  tropopause, 25folding, 390

  troposphere, 24–25, 27, See also free troposphere

  tunable-diode laser (TDL) spectroscopy, 442

  tuning, model. See calibration, model

  turbulence, 8–9, 13, 15, 275cascade, 346

  definition, 5–6

  diffusion, 279

  diffusion coefficient, 351

  diffusion matrix, 351

  eddy flux, 347

  flow regime, 344

  kinetic energy (TKE), 346

  mechanical, 48

  momentum equation, 353

  similarity assumption, 352

  stochastic models. See stochastic models

  turbulent mixing, 105

  two-film model, 401

  two-stream method, 223

  two-way surface exchange, 410

  unimolecular reaction, 229reaction rate, 230

  Van’t Hoff law, 236

  variogram. See kriging

  variational method, 520, 530

  velocity of an air parcel, 36

  of Earth’s rotation, 36

  velocity potential, 111

  ventilation of the planetary boundary layer, 48, 49

  virtual temperature, 29, 353

  VOC-limited regime, 71

  VOCs. See volatile organic compounds

  volatile organic compounds and tropospheric ozone production, 14

  volatile organic compounds (VOCs), 64–67generic oxidation scheme, 66–67

  nomenclature, 65

  semivolatile, 66

  volatility basis set (VBS) approach, 238

  volatility classes, of organic species, 238

  volcanic explosivity index (VEI), 410

  volume mixing ratio. See mixing ratio

  Von Karmann constant, 374

  Von Neumann analysis. See stability

  Voronoi diagram, 189

  vorticity. See curl

  vorticity absolute, 110

  Ertel potential, 112

  potential, 112

  relative, 112

  warm pool, Pacific Ocean, 43

  water vapor atmospheric abundance, 21, 28

  greenhouse gas, 23

  wavelength, 205

  weather forecast model. See meteorological model

  wet chemistry, 439

  wet deposition below-cloud scavenging. See washout

  convective scavenging, 382–384

  in-cloud scavenging. See rainout

  large scale scavenging, 383

  rainout, 383, 385

  retention efficiency, 384

  washout, 383, 385–386

  wet scavenging. See wet deposition

  Wien’s displacement law, 212

  wind shear dimensionless, 375

  Zel’dovich mechanism, 62, 386

  zenith angle, 571

 

 

 


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