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Introduction to tropical meteorology and deep convection Roger K. Smith University of Munich
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Topics
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INDO IR 01010510
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GMS IR 01022621
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GOES IR 00112909
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Principal land and ocean areas between 40°S and 40°N. The shaded areas show tropical highlands (over 1000 m). From Nieuwolt (1977)
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How does one define the tropics? Tropic of Capricorn 23.5 o s Tropic of Cancer 23.5 o N Maritime continent
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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Radiative heat balance Zonally averaged components of the absorbed solar flux and emitted thermal infrared flux at the top of the atmosphere. (after Vonder Haar and Suomi, 1971, with modifications) F (W m 2 ) 100 0 200 300 90 50 30 10 0 10 30 50 90 South Latitude North Absorbed solar flux Emitted infrared flux energy gain energy loss +
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Mean annual precipitation Mean annual precipitation as a function of latitude. (after Sellers, 1965) 2000 1500 1000 500 mm 0 90 60 40 30 20 10 0 10 20 30 40 60 90 North Latitude South
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mean meridional circulation The mean meridional circulation and main surface wind regimes. after Defant, 1958 Hadley circulation
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ITCZ
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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Field Experiments in the Tropics 1969 - 1979 Bermuda Oceanographic and Meteorological EXperiment (BOMEX) 1969 Holland & Rasmusson, (1973), MWR, 101, 44-55. Global Atmospheric Research Programme (GARP) Atlantic Tropical Experiment (GATE) July 1974 GARP: Fleming et al., (1979), BAMS, 60, 649-659. GATE: Kuettner et al. (1974) BAMS, 55, 711-744. The MONsoon EXperiment (WMONEX December 1978, SMONEX May – August, 1979) WMONEX: Greenfield & Krishnamurti (1979), BAMS, 60, 649- 659.SMONEX: Fein & Kuettner (1980) BAMS, 61, 461-474.
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Field Experiments in the Tropics 1987 - Australian Monsoon EXperiment & Equatorial Mesoscale EXperiment (AMEX, EMEX) January – February 1987 AMEX Holland et al. (1986), BAMS, 67, 1466-1486. EMEX Webster & Houze (1991), BAMS, 72, 1481-1505. Tropical Oceans Global Atmosphere Couple Ocean Atmosphere Response Experiment (TOGA COARE) November 1992 – February 1993 Webster & Lucas (1992), BAMS, 73, 1377-1416.
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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850 mb 200 mb JJA
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200 mb 850 mb DJF
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Velocity potential We can separate the three-dimensional velocity field into a rotational part and a divergent part (see e.g. Holton, 1972, Appendix C.) rotational nondivergent irrotational divergent
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Upper tropospheric (200 mb) mean seasonal velocity potential indicating the divergent part of the mean seasonal wind which is proportional to . (Adapted from Krishnamurti et al., 1973).
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OLR < 225 W m 2 month From Lau & Chan, 1983
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Walker circulation
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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Monsoons July
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SE Asian Monsoon
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January
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Australasian Monsoon
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South America: January climatology 200 mb wind850 mb wind
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(From Webster, 1983) An example of monsoon variability 1963 1971 West coast of India
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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Time-longitude section of vis imagery - latitude band 10 -15 N From Wallace, 1970 July August June 0107 01/06 0108 time
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Fig. 1.23 GMS – IR 25 Dec 1978 MSLP 25 Dec 1978 Winter MONEX A B C From Webster, 1983
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Fig. 1.24 250 mb 25 Dec 1978 850 mb 25 Dec 1978 Winter MONEX A B C A BC shaded horizontal wind divergence From Webster, 1983
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The variation of surface pressure at Darwin for the period 23 - 28 Dec. 1978.
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Easterly waves over Africa WV Imagery 17 June 1997 00Z
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Tropical cyclones TC tracks (1979-1988) Super typhoon Wynnie 11 Aug 1997
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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Moist Convection Trade Cumuli
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The tropical troposphere z km 29 o C -73 o C 15 -121 o C observed -150 o C+150 o C 77 o C Conclusion: Deep tropical circulations cannot be dry adiabatic
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The role of diabatic processes z km 15 Conclusion: Deep convection occupies a small fractional area Latent heat release opposes adiabatic cooling Radiative cooling opposes adiabatic warming ITCZ subtropical high Fast ascent Slow descent
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Successive locations of radar reflectivity contours in a tropical squall line. From Chang et al. (1987) Radar reflectivity contours (dBZ) of a tropical squall line observed during COPT81 (Ivory Coast, West Africa). Horizontal cross-section at low levels (0.5 – 1.5 km).
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Radar reflectivity contours (dBZ) of a tropical squall line observed during COPT81 (Ivory Coast, West Africa). Vertical cross-section along the axis of propagation.
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Types of convection
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A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone (ITCZ) Field experiments Macroscale circulations, The Walker circulation, Monsoons Synoptic scale weather systems, tropical waves Moist convection and convective systems The Madden-Julian Oscillation, Westerly wind bursts Concluding remarks Next topic
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From JAS, Sept. 1972 Madden-Julian Oscillation
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From Webster 1987 Madden-Julian Oscillation MJO
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Indian Ocean Feb/Mar 2001 06/0207/0213/02 17/0224/0206/03
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West Pacific Ocean – Feb 2001 06/0209/0213/02 21/0224/0229/02
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http://www.bom.gov.au/bmrc/clfor/cfstaff/matw/maproom/OLR/hov.last6mths.anom.S.gif
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GOES-9 12 UTC 2 Dec 1997 10.7 micron image Westerly wind bursts
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Interaction between moist convection and the large-scale flow. What are the controls on deep convection. Models don’t get the diurnal variation correct. No generally accepted theory of the Madden-Julian Oscillation. Weather forecasting in the tropics is still very difficult compared with that in the middle latitudes. A few outstanding problems
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The End Thank you for your interest Talk available at: http://www.meteo.physik.uni-muenchen.de\~roger\030514-dlr.pdf
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