weather discussion 7-5-2011. tropical storm arlene at landfall

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  • Slide 1
  • Weather Discussion 7-5-2011
  • Slide 2
  • Tropical Storm Arlene at Landfall
  • Slide 3
  • Microwave Imagery of Tropical Storm Arlene at Landfall
  • Slide 4
  • Brownsville, TX Radar
  • Slide 5
  • 500-mb Analysis (12Z on 6/30 Thursday Morning)
  • Slide 6
  • U.S. Surface Analysis (12Z on 6/30 Thursday Morning)
  • Slide 7
  • N.C. Surface Analysis (12Z on 6/30 Thursday Morning)
  • Slide 8
  • GSO Sounding (12Z on 6/30 Thursday Morning)
  • Slide 9
  • Dry air aloft (00Z on Thursday)
  • Slide 10
  • 500-mb Analysis (00Z on 7/1 Thursday Evening)
  • Slide 11
  • U.S. Surface Analysis (00Z on 7/1 Thursday Evening)
  • Slide 12
  • N.C. Surface Analysis (00Z on 7/1 Thursday Evening)
  • Slide 13
  • GSO Sounding (00Z on 7/1 Thursday Evening)
  • Slide 14
  • GSO Back Trajectories (00Z on 7/1 Thursday Evening)
  • Slide 15
  • 500-mb Analysis (12Z on 7/1 Friday Morning)
  • Slide 16
  • U.S. Surface Analysis (12Z on 7/1 Friday Morning)
  • Slide 17
  • N.C. Surface Analysis (12Z on 7/1 Friday Morning)
  • Slide 18
  • GSO Sounding (12Z on 7/1 Friday Morning)
  • Slide 19
  • Visible Satellite Imagery (Friday Afternoon at 2:00PM)
  • Slide 20
  • Water Vapor Imagery (Friday Afternoon at 2:00PM)
  • Slide 21
  • IR Satellite Imagery (Friday Afternoon at 4:00PM)
  • Slide 22
  • A little bit about transverse cirrus bands The ideal case for band production appeared to be a strong, isolated convective system that developed, matured, and dissipated without interacting with any other convective storm (Lenz et al. [2009], 1365). Transverse bands were more commonly observed to emerge near the end of the mature stage of the [convective] system and persist through the decay stage of the system (Lenz et al. [2009], 1365). Transverse bands were observed at all hours of the day, though they were most common during the nighttime hours of this study (Lenz et al. [2009], 1368). The average time lag between convection initiation and the first observation of transverse bands was 7 hours, and the average duration of the bands was about 9 hours (Lenz et al. [2009], 1369, 1372). Most commonly develop in regions of upper-level divergence and a strong relative vorticity gradient
  • Slide 23
  • Geographic Distribution (May August 2006) Lenz et al. (2009) pg. 1368
  • Slide 24
  • Transverse Bands and Aviation Turbulence Lenz et al. (2009) pg. 1364
  • Slide 25
  • 500-mb Analysis (00Z on 7/2 Friday Evening)
  • Slide 26
  • U.S. Surface Analysis (00Z on 7/2 Friday Evening)
  • Slide 27
  • N.C. Surface Analysis (00Z on 7/2 Friday Evening)
  • Slide 28
  • GSO Sounding (00Z on 7/2 Friday Evening)
  • Slide 29
  • GSO Back Trajectories (00Z on 7/2 Friday Evening)
  • Slide 30
  • 500-mb Analysis (12Z on 7/2 Saturday Morning)
  • Slide 31
  • U.S. Surface Analysis (12Z on 7/2 Saturday Morning)
  • Slide 32
  • N.C. Surface Analysis (12Z on 7/2 Saturday Morning)
  • Slide 33
  • GSO Sounding (12Z on 7/2 Saturday Morning)
  • Slide 34
  • 500-mb Analysis (00Z on 7/3 Saturday Evening)
  • Slide 35
  • U.S. Surface Analysis (00Z on 7/3 Saturday Evening)
  • Slide 36
  • N.C. Surface Analysis (00Z on 7/3 Saturday Evening)
  • Slide 37
  • GSO Sounding (00Z on 7/3 Saturday Evening)
  • Slide 38
  • GSO Back Trajectories (00Z on 7/3 Saturday Evening)
  • Slide 39
  • 500-mb Analysis (12Z on 7/3 Sunday Morning)
  • Slide 40
  • U.S. Surface Analysis (12Z on 7/3 Sunday Morning)
  • Slide 41
  • N.C. Surface Analysis (12Z on 7/3 Sunday Morning)
  • Slide 42
  • GSO Sounding (12Z on 7/3 Sunday Morning)
  • Slide 43
  • 500-mb Analysis (00Z on 7/4 Sunday Evening)
  • Slide 44
  • U.S. Surface Analysis (00Z on 7/4 Sunday Evening)
  • Slide 45
  • N.C. Surface Analysis (00Z on 7/4 Sunday Evening)
  • Slide 46
  • GSO Sounding (00Z on 7/4 Sunday Evening)
  • Slide 47
  • GSO Back Trajectories (00Z on 7/4 Sunday Evening)
  • Slide 48
  • 500-mb Analysis (12Z on 7/4 Monday Morning)
  • Slide 49
  • U.S. Surface Analysis (12Z on 7/4 Monday Morning)
  • Slide 50
  • N.C. Surface Analysis (12Z on 7/4 Monday Morning)
  • Slide 51
  • GSO Sounding (12Z on 7/4 Monday Morning)
  • Slide 52
  • Visible Satellite Imagery (Monday Afternoon at 4:45PM)
  • Slide 53
  • IR Satellite Imagery (Monday Afternoon at 4:45PM)
  • Slide 54
  • Water Vapor Imagery (Monday Afternoon at 4:45PM)
  • Slide 55
  • Visible Satellite Imagery (Monday Evening at 6:45PM)
  • Slide 56
  • IR Satellite Imagery (Monday Evening at 6:45PM)
  • Slide 57
  • Water Vapor Imagery (Monday Evening at 6:45PM)
  • Slide 58
  • Total Precipitation for July 4th
  • Slide 59
  • 500-mb Analysis (00Z on 7/5 Monday Evening)
  • Slide 60
  • U.S. Surface Analysis (00Z on 7/5 Monday Evening)
  • Slide 61
  • N.C. Surface Analysis (00Z on 7/5 Monday Evening)
  • Slide 62
  • GSO Sounding (00Z on 7/5 Monday Evening)
  • Slide 63
  • GSO Back Trajectories (00Z on 7/5 Monday Evening)
  • Slide 64
  • 500-mb Analysis (12Z on 7/5 Tuesday Morning)
  • Slide 65
  • U.S. Surface Analysis (12Z on 7/5 Tuesday Morning)
  • Slide 66
  • N.C. Surface Analysis (12Z on 7/5 Tuesday Morning)
  • Slide 67
  • GSO Sounding (12Z on 7/5 Tuesday Morning)
  • Slide 68
  • Visible Satellite Imagery (Tuesday Morning at 8:30AM)
  • Slide 69
  • IR Satellite Imagery (Tuesday Morning at 8:30AM)
  • Slide 70
  • Water Vapor Imagery (Tuesday Morning at 8:30AM)
  • Slide 71
  • Sizzlin Savannah Savannah Area (ThreadEx Station)ThreadEx Station) Consecutive Days Maximum Temperature >= 90.0 degrees F Years: 1874-2011 Rank # Days End Date 1 46 7/ 4/2011 2 44 8/ 8/1993 3 40 8/14/2010 4 36 7/27/1932 5 34 8/22/1999 End Date is the last day of the run. This station's record may include data from more than one, possibly incompatible, locations. It reflects the longest available record for the Savannah Area.
  • Slide 72
  • Soggy Forecast???