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1
Kenneth E. Kunkel
NOAA Cooperative Institute for Climate and Satellites, North
Carolina State University
Historical Perspective on
Hurricane Harvey Rainfall
2
Hurricane Harvey
• One focus of working group
o Late August 2017
o Multi-day rainfall exceeded 50 inches in some
locations
o This reached Probable Maximum Precipitation
levels
o Massive flooding
3
4
Physics and Statistics/Math
• Phenomenology-centric view of extreme
precipitation events
5
Meteorology of Observed Extremes
Dominated by large systems
6
Extreme Precipitation – climate analysis
• Define an overlapping grid of cells separated by 1/10 degree in latitude and 1/10
degree in longitude covering longitudes 80–100°W and latitudes 25–35 °N (large
blue box on following figure).
• Within the grid, consider all possible 2-degree by 2-degree boxes (all boxes like the
red box in the figure). This represents an approximate area of 40,000 km2.
• Compute daily precipitation for 1949-present as a simple average of all stations in
each box. All boxes that are wholly or partly over water are not included in this
analysis.
• For each grid box, identify top 5-day precipitation totals.
• Pool everything together and identify the top 100 events for 1949–2017 across the
entire region, ignoring those that overlap in time or space with larger event.
• Rank and plot these.
• Also did same analysis on other grid sizes from 1° to 3°
7
Grid box lattice
8
Ranking of 2° x 2° events
Harvey
9
2° x 2° event locations
10
Ranking of 1° x 1° events
Harvey
11
1° x 1° event locations
12
Ranking of 3° x 3° events
Harvey
13
3° x 3° event locations
14
Meteorological Causes
• For 2° to 2° “top 100” events:
– 24 were caused by tropical cyclones
– Most of rest were associated with fronts
15
Monthly Distribution - 2° to 2° events
16
Top 100 Gulf Region Events
17
• Complex temporal and spatial coherence and
variability of extreme precipitation events –
– Individual thunderstorm cells – hour, a few km
– Thunderstorm complexes – a few hours, tens-100+ km
– Spiral rain bands in hurricanes – a few hours, tens-
100+ km
– Low pressure wave – day, 100s of km
– Hurricanes – day, 100s of km
– Synoptic low pressure system – days, 1000+ km
– Hemispheric jet stream wave patterns – weeks, 1000s
of km
The Challenge
17
18
• Weather system based inquiry of historical
trends and future changes
– Statistical trend significance tests
– Automated tools
– How do we incorporate this approach into the
standard statistical approaches for estimating
design values
Research
18
19
Basic Elements of PMP
20
Annual Maximum 24-hr Upward Motion
21
Questions?

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Climate Extremes Workshop - Historical Perspective on Hurricane Harvey Rainfall - Ken Kunkel, May 16, 2018

  • 1. 1 Kenneth E. Kunkel NOAA Cooperative Institute for Climate and Satellites, North Carolina State University Historical Perspective on Hurricane Harvey Rainfall
  • 2. 2 Hurricane Harvey • One focus of working group o Late August 2017 o Multi-day rainfall exceeded 50 inches in some locations o This reached Probable Maximum Precipitation levels o Massive flooding
  • 3. 3
  • 4. 4 Physics and Statistics/Math • Phenomenology-centric view of extreme precipitation events
  • 5. 5 Meteorology of Observed Extremes Dominated by large systems
  • 6. 6 Extreme Precipitation – climate analysis • Define an overlapping grid of cells separated by 1/10 degree in latitude and 1/10 degree in longitude covering longitudes 80–100°W and latitudes 25–35 °N (large blue box on following figure). • Within the grid, consider all possible 2-degree by 2-degree boxes (all boxes like the red box in the figure). This represents an approximate area of 40,000 km2. • Compute daily precipitation for 1949-present as a simple average of all stations in each box. All boxes that are wholly or partly over water are not included in this analysis. • For each grid box, identify top 5-day precipitation totals. • Pool everything together and identify the top 100 events for 1949–2017 across the entire region, ignoring those that overlap in time or space with larger event. • Rank and plot these. • Also did same analysis on other grid sizes from 1° to 3°
  • 8. 8 Ranking of 2° x 2° events Harvey
  • 9. 9 2° x 2° event locations
  • 10. 10 Ranking of 1° x 1° events Harvey
  • 11. 11 1° x 1° event locations
  • 12. 12 Ranking of 3° x 3° events Harvey
  • 13. 13 3° x 3° event locations
  • 14. 14 Meteorological Causes • For 2° to 2° “top 100” events: – 24 were caused by tropical cyclones – Most of rest were associated with fronts
  • 15. 15 Monthly Distribution - 2° to 2° events
  • 16. 16 Top 100 Gulf Region Events
  • 17. 17 • Complex temporal and spatial coherence and variability of extreme precipitation events – – Individual thunderstorm cells – hour, a few km – Thunderstorm complexes – a few hours, tens-100+ km – Spiral rain bands in hurricanes – a few hours, tens- 100+ km – Low pressure wave – day, 100s of km – Hurricanes – day, 100s of km – Synoptic low pressure system – days, 1000+ km – Hemispheric jet stream wave patterns – weeks, 1000s of km The Challenge 17
  • 18. 18 • Weather system based inquiry of historical trends and future changes – Statistical trend significance tests – Automated tools – How do we incorporate this approach into the standard statistical approaches for estimating design values Research 18
  • 20. 20 Annual Maximum 24-hr Upward Motion