Coastal Meteorology - Institute of Coastal Research

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Theory Breakdown in the Coastal Zone Normally: similarity theory after Monin-Obukhov provides model for fluxgradient relationship in surface layer ... but: sign. vertical divergence of flux due to strong horiz. advection, no height independent fluxes U 10 often to high in internal boundary layer offshore flow often warm air over cold water ⇒ upside down convection turbulence often not in equilibrium (fetch, time) ... more: Mahrt 1999 M.Quante 2002
Some references on Air-Sea-Exchange: Atmosphere-Ocean Interaction (Oxford Monographs on Geology and Geophysics, No 27) by Eric B. Kraus, Joost A. Businger (1994) Air-Sea Exchange: Physics, Chemistry and Dynamics (Kluwer Academic Publishers, Atmospheric and Oceanographic Sciences Library, 578pp) by Gerald L. Geernaert (Editor) (1999) M.Quante 2002
Page 1 and 2: Coastal Meteorology Markus Quante G
Page 3 and 4: Introduction • Coastal zones belo
Page 5 and 6: Coastal Zone from LOICZ (Land Ocean
Page 7 and 8: Scope of Coastal Meteorology Defini
Page 9 and 10: Examples of coastal meteorological
Page 11 and 12: Who is interested in CM ? predictio
Page 13 and 14: Meteorology science dealing with th
Page 15 and 16: Meteorological scales here: horizon
Page 17 and 18: Meteorological Elements Basic physi
Page 19 and 20: Coriolis Force (an artifact of the
Page 21 and 22: Gradient Wind non-geostrophic winds
Page 23 and 24: The Atmospheric Boundary Layer The
Page 25 and 26: height z [m] 10 4 10 3 10 2 10 1 10
Page 27 and 28: The Logarithmic Wind Profile (horiz
Page 29 and 30: M.Quante 2002
Page 31 and 32: from Rotunno et al., 1992 Real Prof
Page 33 and 34: Internal boundary layer due to temp
Page 35 and 36: Air-Sea Exchange Atmosphere and oce
Page 37 and 38: Processes governing heat, mass and
Page 39 and 40: w′ Fluxes and bulk formulas ⎛
Page 41: from Rotunno et al., 1992 M.Quante
Page 45 and 46: Land/Sea Breeze Sea/Land Breeze has
Page 47 and 48: Sea Breeze qualitative calm atmosph
Page 49 and 50: Circulation integral measure of rot
Page 51 and 52: M.Quante 2002
Page 53 and 54: In reality often much more complex
Page 55 and 56: Plant and Atkinson, 2002 Offshore w
Page 57 and 58: European example / North-Sea N V U
Page 59 and 60: Florida Sea breeze Complex land-sea
Page 61 and 62: Coastal Fronts A longer-lived cousi
Page 63 and 64: Meso-low Low Level Jet from Raman e
Page 65 and 66: The influence of orography Coastal
Page 67 and 68: Localized regions of high or low pr
Page 69 and 70: Coastally-trapped disturbances that
Page 71 and 72: Trapped Phenomena damming Upstream
Page 73 and 74: Trapped Phenomena Moderate Froude N
Page 75 and 76: Land-falling storms example hurrica
Page 77 and 78: Air quality aspects (nutrient trans
Page 79 and 80: Air quality aspects (sea/lake breez
Page 81 and 82: Coastal lows and sulfur air polluti
Page 83 and 84: Coastal Clouds → Radiaton → pre
Page 85 and 86: Coastal Clouds (sea breeze front, e
Page 87 and 88: Ground based platforms M.Quante 200
Page 89 and 90: Advanced moving platforms M.Quante
Page 91 and 92: Radiometers in the field M.Quante 2
Page 93 and 94:
Wind profiler at Cabauw, NL profile
Page 95 and 96:
Height [km] 12 10 8 6 4 2 12.4 12.6
Page 97 and 98:
Grafik: EarthCare Science Team ESA
Page 99 and 100:
Heat flux in marine boundary layer
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Coastal Meteorology - Institute of Coastal Research

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