You might have seen a WDAY weather promotion on television talking about how we use the Dual-Pol Doppler technology. The promotion, however, does not get into what this thing is. Dual-Pol is short for Dual-Polarity Doppler. The National Weather Service Doppler system, including the one at Mayville, ND, now sends out two Doppler pulses oriented perpendicularly. This allows a set of computer algorithms to make some assumptions about the shapes of the objects it “sees.” One key advantage we used extensively a week ago is the ability to discern between snowflakes and raindrops. Traditional Doppler could not do that. Another function is the ability to detect storm debris as a way of confirming if a tornado is actually causing damage. Both of these functions are limited by the fact that the Doppler beam is at a certain height above the ground and cannot always “see” what is actually right at ground level. Meteorologist John Wheeler
In the space of thirteen days, from May 6 to May 18, Fargo Moorhead’s annual precipitation total to the date went from the 17th driest on record to the 15th wettest . The 5.82 inches of rain that fell those thirteen days alone would rank in 8th place on the list of wettest Mays. And yet there was hardly any river flooding in the entire region. Sure there has been some minor lowland flooding in the typical flood prone areas, the sort of flooding that is common after heavy rain. But nowhere in our region has there been any of the significant flooding one would expect following such a rain. Most of the fields that had standing water for a few days have dried nicely, suggesting additional water storage capacity if needed. We can thank the fall-winter-early spring drought for this. Meteorologist John Wheeler
Rainfall and heavy rainfall go together. That is, when there is a pattern of above-average and more frequent rainfall, it is also more likely that there will be a downpour. Warm weather and heavy rainfall also go together. When the atmosphere is warmer, there is more capacity to hold moisture in the air, which increases the potential for downpours. As the average temperature in our region has risen since the middle of the 1900s, so has the frequency of heavy rains. Also, as the average annual precipitation began to rise in the 1990s, the downpours have been increasing. The flooding problem across our region the past 20 years can be tied to both of these trends. The future of flooding in our region is likely going to be tied to both of these trends. Additional warming appears likely but a further increase in annual precipitation is probably less likely. Meteorologist John Wheeler
Although the interior of the Antarctic continent is getting colder, one of the most rapidly warming locations on Earth the past few decades is along the Antarctic Peninsula. An ice shelf known as Larsen C, the fourth largest ice shelf in the world at more than 20,000 square miles, adjoins the Antarctic Peninsula and has been discovered to be melting at a rapid rate due to the warmer air temperatures and the warmer seas underneath. A research team from the British Antarctic Survey has reported a growing crack in the shelf which could cause it to break up some time in the next 100 years. This would not lead directly to a rise in sea levels because this ice is already floating in the ocean. However, if the region continues to warm, the loss of the ice shelf could allow glaciers presently land locked to melt into the ocean faster. Sea-level rise is one of the greatest concerns associated with Global Warming. John Wheeler
Tree ring analysis suggests the present drought in the Southwestern U.S. may be the fourth most severe in approximately the past 1000 years. The nation’s two largest reservoirs, Lake Powell and Lake Mead, both on the Colorado River, are at their lowest levels since construction. These two impoundments provide much of the water needs for desert metropolises such as Las Vegas and Phoenix. This melted snow also provides considerable water for the Los Angeles Basin and the California agriculture industry, which is where a large portion of America’s grocery store produce is grown. The lakes are at approximately 40 per cent of capacity this spring, and will drop more over the summer. Hopefully, next winter’s El Nino will help generate an above-average snow pack in the Rockies next winter or the situation will continue to worsen. Meteorologist John Wheeler
There are three major, large-scale factors which can have large scale effects on the Atlantic hurricane season. One is the general sea-surface temperature. If the tropical part of the Atlantic Basin is warmer than average, there is more thermodynamic energy available for hurricanes. Another is the amount of dust from the Sahara. Actually, it isn’t the dust, but the deep layer of dry air which accompanies these dust clouds that rob tropical storms of moisture. The other key is the overall strength of upper level winds. When the winds aloft are strong, tropical storms tend to shear apart before they can grow large and powerful. The presence of a building El Nino such as there is at present often produces stronger winds above the Atlantic, usually signaling a quieter Atlantic hurricane season. Meteorologist John Wheeler
The cold weather earlier this week prompted many inquiries as to the relative unusualness of having snow and temperatures so cold in the middle of May. Fargo did set a daily record cold maximum temperature Monday at 40 degrees. Old record was 44 set in 1890. May snowfall is also rare, but not without precedent. I would describe such weather in our region as rare, but not unusual; the sort of thing that happens every few years or so. The most unusually wintry May weather on record in the Fargo Moorhead area was in 1907. There was measurable snow in Fargo on four separate days; the 2nd, 13th, 14th, and 19th; for a total of 4.2 inches. The first ten mornings in May were all in the 20s (except for May 2 when it was 17). There were three more hard freeze mornings on the 14th, 20th, and 27th. Meteorologist John Wheeler
It was just one week ago that it started raining. Rain over the seven days since has been plentiful enough to eliminate all concern about it being dry. It is interesting to note that our weather condition can switch from dry to wet in such a short time. On the other hand, it cannot switch from wet to dry so quickly. Of course, it can stop raining tomorrow, but the lingering effects of recent rain will keep the soil soggy and the grass growing for some time. The winter drought began last September 5. That was the day after the last heavy rain of 2014. We were in a drought through the fall because the drier weather caused us no problems. The drought really began to manifest itself this spring with agriculture’s need for germinating rainfall along with a rash of grass fires. Now suddenly, all that is over. I wonder when the next drought will begin. Tomorrow, perhaps?
Meteorologist John Wheeler
The average daily high temperature is not meant to be a reflection of what the temperature is supposed to be. Rather, it is the average of all the daily highs over a period of record. So with that in mind, the average daily high has now reached 70 degrees for the first time since September. There have already been 17 days with a high temperature of at least 70 degrees this year. The first was back on March 15. It happened 11 times during a warm, dry April. The warmest has been 87 degrees on May 2. We had a lot of warmer than average afternoons from mid-March through early May due to the early snowmelt and exposed dry soils. Now that the ground is wet, it will become a little harder to get so many above average afternoon temperatures. Unless, of course, it stops raining again and the ground becomes dry. Meteorologist John Wheeler
Is our warming climate effect the threat of tornadoes and severe thunderstorms? From the political sides of this debate, this question can be quickly and easily answered either “Yes!” or “No!” depending on the politics. In the real world, the answer is a lot trickier. The trend across the United States in recent decades is a decrease in the overall number of tornado days along with an overall decrease in the quantity of tornadoes. But coupled with this decrease in bad storms is an increase in those few terrible tornado outbreak days, those days when dozens or even hundreds of tornadoes causing staggering property damage and loss of life. So although severe storms are not exactly increasing, their variability is. Some of this statistical clustering is skewed by the year, 2011, when several huge tornado outbreaks swept the Midwest and South. Ongoing research offers no consensus yet of how tornadoes will be affected by climate change in the future.
Meteorologist John Wheeler