Presentation by John Nielson-Gammon, State Climatologist and Professor of Atmospheric Science at Texas A&M University, at the 2018 Gulf Coast Water Conservation Symposium in Houston, Texas.
5. (Central/Eastern) US Depth-Area-Duration
All-Time Records Before Harvey
John Nielsen-Gammon, Texas A&M University 5
AreaDuration 2 Days 3 Days 4 Days 5 Days
1,000 sq mi
Louisiana,
August 1940
Louisiana,
August 1940
Louisiana,
August 1940
Louisiana,
August 1940
2,000 sq mi
Louisiana,
August 1940
Louisiana,
August 1940
Louisiana,
August 1940
Louisiana,
August 1940
5,000 sq mi
Louisiana,
August 1940
Texas,
June 1899
Texas,
June 1899
Texas,
June 1899
10,000 sq mi
Georges,
Florida 1998
Texas,
June 1899
Texas,
June 1899
Texas,
June 1899
20,000 sq mi
Georges,
Florida 1998
Beulah,
Texas 1967
Beulah,
Texas 1967
Beulah,
Texas 1967
50,000 sq mi
Georges,
Florida 1998
Beulah,
Texas 1967
Beulah,
Texas 1967
Beulah,
Texas 1967
6. AreaDuration 2 Days 3 Days 4 Days 5 Days
1,000 sq mi
Louisiana,
August 1940 Harvey Harvey Harvey
2,000 sq mi Harvey Harvey Harvey Harvey
5,000 sq mi Harvey Harvey Harvey Harvey
10,000 sq mi Harvey Harvey Harvey Harvey
20,000 sq mi Harvey Harvey Harvey Harvey
50,000 sq mi Harvey Harvey Harvey Harvey
(Central/Eastern) US Depth-Area-Duration
All-Time Records After Harvey
John Nielsen-Gammon, Texas A&M University 6
13. John Nielsen-Gammon, Texas A&M University 13
8
10
12
14
16
18
20
22
24
1946 1956 1966 1976 1986 1996 2006 2016
Yearly Maximum Observed 2-Day Rain, Long-Term
Sta ons, Harris County
Maximum Observed 2-Day Rain Number of Sta ons Repor ng
32. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 32
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
Increase
33. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 33
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
34. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 34
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
35. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 35
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
36. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 36
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
37. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 37
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
38. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 38
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
39. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 39
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
Historical
40. Drought: Consider the Possibilities
John Nielsen-Gammon, Texas A&M University 40
HeavyRainIntensity
Steady
Total Rainfall Amount
Increase Steady Decrease
X
Increase
/
Historical
Model
Projections
41. Messages
• Harvey was exceptional
• Odds of extreme rainfall have increased
– And will continue to increase
– Odds change ballpark estimate: Factor of 3 (2-8)
per °C global warming
– Amount change ballpark estimate: 15% (10-30%)
per °C global warming
John Nielsen-Gammon, Texas A&M University 41
42. More Messages
• Annual rainfall amounts have increased
– But may decrease in future
• Future drought intensity depends on:
– Intensity of heavy rain
– Overall rainfall amounts
– Increasing temperatures (a given)
• Houston has been unlucky
John Nielsen-Gammon, Texas A&M University 42
43. Comprehensive Rainfall Survey
(NSF-funded project)
• Data being collected
– Weather & climate (COOP, WBAN)
– Hydrological (HCFCD, LCRA)
– Popular networks (CoCoRaHS, WU)
– Independent “backyard” observers
• Analysts: Texas A&M, AWA, MetStat
• Please share your data!
– http://climatexas.tamu.edu/harvey/survey/
– n-g@tamu.edu
John Nielsen-Gammon, Texas A&M University 43
46. Image: New York Times 2017, with data from NWS, NASA GEOS, and IBTRACS
Harvey’s corral radius: 123 km centered at 12 UTC Aug 27
Average maximum sustained wind while stalled: 50 kt (26 m/s)
47. How Slow Can Tropical Cyclones Go?
0
5
10
15
20
25
30
35
0 200 400 600 800 1000 1200 1400 1600 1800
NumberofStorms
Smallest Corral Radius (km) for Each Storm
“Stalling”: 1 in 7.4
49. 50
75
100
125
150
175
200
0 20 40 60 80 100 120
CorralRadius(km)
Average Wind Speed (kt)
200-400 inland 100-200 inland 0-100 inland 0-50 offshore
50-100 offshore 100-150 offshore 150-200 offshore
Coastal Stalls At Least As Slow and
Intense As Harvey
Flora
1963
5 Days
1910
Mitch
1998
Harvey
2017
One of 2 costliest
Atlantic storms ever
One of 5 deadliest
known Atlantic storms
One of 5 deadliest
known Atlantic storms
52. Number of Coastal Stalls:
100 km inland to 50 km offshore
0
2
4
6
8
Other
Cuba
Mex/CentAm
USA
53. Probability of Harvey Rain
• Probability of strong stall
• Conditional probability of moisture channel
John Nielsen-Gammon, Texas A&M University 53
55. Probability (per century) of Strong Stall
in 1°x1° Box
• 1917-2017: 0.08
• 1967-2017: 0.13
• Superstall (<100 km): 0.02
John Nielsen-Gammon, Texas A&M University 55
56. 0
5
10
15
20
25
30
35
40
45
50
1000 10000 100000
PrecipitationDepth(In)
Storm Area (Sq. Mile)
Comparison Between Harvey and
Probable Maximum Precipitation
Harvey 48-hr
PMP 48-hr
Harvey 72-hr
PMP 72-hr
Lines being below the square boxes means that Harvey did not exceed
the previously estimated Probable Maximum Precipitation for the Gulf region
Graphic by David Maidment, University of Texas at Austin
John Nielsen-Gammon, Texas A&M University 56