Colorado State University

Seasonal Hurricane Forecasting

Atlantic Seasonal Hurricane Activity

Forecast for 2020 Hurricane Activity (as of August 5, 2020)

Forecast Parameters CSU Forecast for 2020* Average for 1981-2010
Named Storms 24 12.1
Named Storm Days 100 59.4
Hurricanes 12 6.4
Hurricane Days 45 24.2
Major Hurricanes 5 2.7
Major Hurricane Days 11 6.2
Accumulated Cyclone Energy+ 200 106
*Total forecast includes Arthur, Bertha, Cristobal, Dolly, Edouard, Fay, Gonzalo, Hanna and Isaias which have formed in the Atlantic as of August 4th.
+A measure of a named storm’s potential for wind and storm surge destruction defined as the sum of the square of a named storm’s maximum wind speed (in 104 knots2) for each 6-hour period of its existence.

We have increased our forecast and now call for an extremely active 2020 Atlantic hurricane season.

Sea surface temperatures averaged across the tropical Atlantic are much warmer than normal, and vertical wind shear is well below average. Current cool neutral ENSO conditions may transition to weak La Niña conditions by later this summer. We anticipate an above-normal probability for major hurricanes making landfall along the continental United States coastline and in the Caribbean.

As is the case with all hurricane seasons, coastal residents are reminded that it only takes one hurricane making landfall to make it an active season for them. They should prepare the same for every season, regardless of how much activity is predicted.

Read the full document

2020 CSU Tropical Meteorology Project Forecast Schedule

Two-week Forecasts of North Atlantic Tropical Cyclone Activity

Real-time statistics calculated from operational best tracks of NHC, CPHC and JTWC

Real-Time Tropical Cyclone Statistics





Global Tropical Cyclone Activity for 2020 (2020/2021 for the Southern Hemisphere)

1981-2010 Climatological Activity Through 15 August in Parentheses
Basin Named Storms Named Storm Days Hurricanes Hurricane Days Major Hurricanes Major Hurricane Days Accumulated Cyclone Energy
North Atlantic 11 (3.1) 27.0 (9.8) 2 (0.9) 3.0 (2.2) 0 (0.3) 0 (0.4) 25.1 (12.4)
Northeast Pacific 5 (8.0) 19.25 (33.2) 2 (4.0) 7.0 (12.6) 1 (1.9) 2.0 (3.6) 33.0 (57.1)
Northwest Pacific 7 (10.7) 12.0 (48.3) 3 (6.2) 3.0 (20.4) 1 (2.9) 0.5 (6.9) 13.8 (94.6)
North Indian 2 (1.8) 5.75 (5.7) 2 (0.6) 4.0 (1.4) 1 (0.4) 2.25 (0.6) 19.2 (8.2)
Northern Hemisphere 25 (23.6) 64.0 (97.0) 9 (11.7) 17.0 (36.6) 3 (5.5) 4.8 (11.5) 91.1 (172.3)
South Indian 0 (0.3) 0 (0.4) 0 (0.0) 0 (0.0) 0 (0.0) 0 (0.0) 0 (0.2)
South Pacific 0 (0.0) 0 (0.0) 0 (0.0) 0 (0.0) 0 (0.0) 0 (0.0) 0 (0.0)
Southern Hemisphere 0 (0.3) 0.0 (0.4) 0 (0.0) 0.0 (0.0) 0 (0.0) 0.0 (0.0) 0.0 (0.2)



Individual Basin Tropical Cyclone Activity for 2020 (2020/2021 for the Southern Hemisphere)


Real-Time North Atlantic Ocean Statistics by Storm for 2020

Storm # Name Active Dates Intensity
(kts)
MSLP
(hPa)
Named
Storm
Days
Hurricane
Days
Major
Hurricane
Days
Accumulated
Cyclone
Energy
1 ARTHUR 5/17 - 5/19 2020 50 991 2.5 0 0 1.75
2 BERTHA 5/27 - 5/27 2020 45 1007 0.5 0 0 0.36
3 CRISTOBAL 6/2 - 6/8 2020 50 992 4.75 0 0 3.45
4 DOLLY 6/23 - 6/24 2020 40 1002 1.0 0 0 0.56
5 EDOUARD 7/6 - 7/6 2020 40 1005 1.0 0 0 0.57
6 FAY 7/9 - 7/11 2020 50 998 1.5 0 0 1.1
7 GONZALO 7/22 - 7/25 2020 55 997 3.5 0 0 2.78
8 HANNA 7/24 - 7/26 2020 75 973 3.0 0.75 0 3.38
9 ISAIAS 7/30 - 8/4 2020 75 987 6.0 2.25 0 9.19
10 JOSEPHINE 8/13 - 8/15 2020 40 1005 2.25 0 0 1.33
11 KYLE 8/14 - 8/15 2020 45 1000 1.0 0 0 0.65


North Atlantic Ocean storm statistics were last modified: 09:00 MDT 2020-08-15. Statistics calculated from global repository data graciously provided by NCAR RAL Tropical Cyclone Guidance Project.


DESCRIPTION OF CLIMATE FACTORS INFLUENCING ATLANTIC HURRICANE ACTIVITY

Forecast Factors

In 1984, Dr Bill Gray at Colorado State University documented that Atlantic hurricane activity responded to a variety of large-scale atmospheric and oceanic parameters spanning various portions of the globe. These large-scale factors interact with the global climate system in such a way that then alter the environment of the tropical Atlantic, where most major hurricanes develop and intensify. For example, hurricanes are more likely to develop when they traverse through an environment of low vertical wind shear (the change in wind direction and speed with height in the atmosphere), high sea surface temperatures and high mid-level moisture. Several parameters that have been documented to impact Atlantic hurricanes are discussed here in more detail.

Atlantic Ocean Thermodynamics

A warmer-than-normal tropical North Atlantic Ocean is known to typically create conditions more favorable for hurricane formation and intensification. In addition to enhancing latent and sensible heat fluxes that fuel tropical cyclones, a warmer tropical North Atlantic also drives lower pressures and reduced low-level trade winds, which also feed back to a more conducive environment for hurricanes.

It is important to note that the warming of the tropical North Atlantic Ocean also be measured relative to warming in other areas. One frequently utilized metric is relative sea surface temperature, which measures the difference between tropical North Atlantic Ocean sea surface temperatures and sea surface temperatures in the rest of the tropics (Vecchi et al. 2008). This index is important because it dictates where anomalous rising and sinking motion is likely to occur. When the tropical North Atlantic Ocean is anomalously warmer than the remainder of the tropics, anomalous rising motion is likely in this area, favoring enhanced tropical cyclone activity.

Averaged sea surface height anomalies measured by Jason 2 in the Pacific Ocean, observed at the beginning of October 2015. Credit: NASA

An additional index that is often utilized to assess the favorability of the tropical North Atlantic Ocean is the Atlantic Meridional Mode (AMM) (Kossin and Vimont 2007). The AMM assesses both the thermodynamic and dynamic state of the tropical North Atlantic Ocean through analysis of low-level winds as well as sea surface temperatures. A positive phase of the AMM is associated with a warmer tropical North Atlantic relative to the tropical South Atlantic, as well as with reduced trade winds in the tropical North Atlantic. Positive phases of the AMM are generally characterized by above-normal Atlantic hurricane activity.

El Niño Southern Oscillation

At the interannual timescale, the prime driver of Atlantic tropical cyclone variability is generally considered to be El Niño Southern Oscillation (ENSO). ENSO is driven by changes in ocean temperature in the tropical Pacific, where above average conditions (El Niño) in the Central and Eastern Pacific shift the convective activity in the tropical Pacific eastward, and modify the Walker cell throughout the tropics. The influence of ENSO on Atlantic tropical cyclone activity is well documented and is understood to occur mainly through local changes in vertical wind shear: during El Niño (La Niña) conditions, the eastward (westward) shift in convection in the tropical Pacific leads to anomalous upper-level westerlies (easterlies) over the Atlantic, which then increases (decreases) the vertical wind shear, thus decreasing (increasing) tropical cyclone activity.

Dust streaming from Mauritania, Senegal, western Sahara and maybe other countries farther East, and heading West toward South America and the Gulf of Mexico. Composite image made with data from VIIRS acquired by Aqua/MODIS on June 24, 2014. Credit: NASA

Sahel Precipitation

Changes in convective precipitation over the Sahel region has been shown to impact zonal winds in the upper-troposphere, which in turn modulate vertical wind shear over the Main Development Region and influence the conditions of cyclogenesis over the tropical Atlantic. It is possible that changes in the nature of the African Easterly Waves coming off the African continent might also be playing a role. Years with higher Sahel rainfall tend to be associated with more active hurricane seasons. The influence of the Sahel precipitation is mostly felt when the thermodynamical conditions over the tropical Atlantic are not conducive to hurricane formation.

Saharan Dust

Dust outbreaks from West Africa impact tropical cyclone activity by reducing Atlantic tropical sea surface temperatures ahead of the hurricane season. Episodes of dust outbreak are also associated with extremely dry air coming from the Sahara, another factor detrimental to cyclone formation.



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