Indications continue to point toward a building El Niño, a pattern that can greatly impact the second half of the hurricane season.
El Niño is part of the El Niño Southern Oscillation (ENSO), which represents a cyclical variation in sea-surface temperatures over the tropical Pacific Ocean.
During the El Niño phase, water is warmer than average in the tropical Pacific. During the La Niña phase, like the past two winters, water is colder than average over the same area.
Both phases of ENSO, along with other factors, can have profound effects on weather patterns around the globe. Although the numbers of both are nearly equal, there are slightly more La Niña than El Niño patterns on record. The strength of both can vary significantly from one similar phase to another.
Simply put, during an El Niño, air is generally rising over the tropical Pacific and generally sinking over the tropical Atlantic.
More technically, wind shear is generally lower on the Pacific side and often higher on the Atlantic side, based on the setup of strong steering winds high in the atmosphere known as the jet stream.
Rising air and low wind shear favors tropical storm and hurricane development, while sinking air and wind shear inhibits it.
Depending on how quickly El Niño develops, there could be a quick shutdown of tropical systems during the latter part of the Atlantic season and tropical cyclones galore and an extended season on the Pacific side.
According to Tropical Weather Expert Dan Kottlowski, "We continue in a lull of activity in the Atlantic now, but not necessarily from a developing El Niño."
This graph shows Tropical Pacific sea-surface temperatures since 1950. Warmer-than-average temperatures show up in red, while cooler-than-average temperatures show up in blue. Neutral ENSO conditions continue at present according to the National Oceanic and Atmospheric Administration's Earth System Research Laboratory. However, there is definitely a warming trend occurring.
"During much of July, we usually see a rather routine separation of the main jet stream with the Atlantic, which often results in a quiet period in terms of tropical cyclones," Kottlowski said.
We currently have disrupting dry air, wind shear and cool waters over the tropical Atlantic.
"Since the jet stream has departed to the north, there are no old frontal zones and upper-level disturbances left in the region from which tropical systems typically form earlier in the season," According to Kottlowski.
These features are deposited by the jet stream.
The main driver of tropical systems during the second half of the hurricane season is the flow of disturbances coming off of Africa, which pass near the Cape Verde Islands in the Atlantic.
This part of the season is also called the Cape Verde season.
The disturbances pick up moisture and often intensify as they move westward over the warm tropical Atlantic waters.
The Cape Verde season ramps up during the second half of the summer and reaches a peak in the early autumn. It often results in long-tracking, powerful hurricanes with Andrew, Hugo and Gloria to name a few.
If the pattern continues with the development of El Niño late in the summer and fall, a number of disturbances could tiptoe along across the Atlantic, only to ramp up near the East and Gulf coast of the United States, where waters are generally much warmer than average.
"The strength of the El Niño has to be considered since a strong El Niño will have more effect than a weak one," Kottlowski added.
There is the possibility that the Atlantic season may be truncated somewhat earlier than average this year due to a moderate El Niño forecast by AccuWeather.com.
However, there could be a pack of formidable storms over several weeks spanning August into September, before the full effects of El Niño come into play.
Only if neutral conditions were to persist, or El Niño only reaches a weak status late in the game, then there would be less truncation and perhaps a more typical length of the Atlantic and Pacific hurricane season.
If El Niño were to crank up strongly early on, it could cut into overall numbers of tropical storms and hurricanes, despite already four (tropical storms) through June.
We expect the number of tropical systems to be near-normal by the end of the season factoring in the early-season and likelihood of the mid-August to mid-September spike. With wind shear, dry air and dust issues now and later over the central Atlantic, there is still the danger of near-U.S. coast hurricane formation and impact mid- to late-season.
As temperatures rise through the weekend in the South, so will the risk for heat-related dangers.
While heavy rainfall inundated the Phoenix area with historic flooding, deadly landslides occurred in Japan, claiming dozens of lives.
While a tropical low is expected to brew into Tropical Storm Cristobal this weekend, the East Coast of the U.S. is being monitored for future impacts -- even if the storm remains well offshore.
United States residents may pay higher heating costs this fall as colder air is expected to grip the Rockies and Plains at times and some quick-hitting chilly shots may impact the Northeast.
A swath of soaking rain will slowly shift from the northern Plains to the Canadian Prairies this weekend, making people reach for their umbrellas and heightening concerns for flooding.
While residents will face more disruptions to outdoor activities on Saturday, dry air will push southward across Pittsburgh to end the weekend.
San Lorenzo, Puerto Rico (1906)
103 degrees, hottest ever in Puerto Rico.
East-Central Kentucky (1980)
2-1/2 to 3 inches of rain in 45 minutes. 75 homes were flooded and one was washed off its foundation, ending up blocking a roadway in the community of Beauty (near the WV-KY line). Heavy damage was reported, there including a washed-out bridge.
Wichita Falls, TX (1980)
108 degrees -- new record high for this date, also the 56th day of the last 59 days that they have reached 100 degrees or more.