Ask Dr. Bob: Seems most of the fronts/thunderstorms arrive in Tyler around 5:00am.
No, Sir, not that I know of; the past several have, indeed, arrived at about that time; this is part of the reason why we’ve had very little severe weather thus far this season.
About the only thunderstorm pattern is that there does seem to be a worldwide thunderstorm maxima at about 2200 GMT each day–in other words, late-afternoon here.
By the way, it looks as Thursday morning’s front will be showing up right around daybreak.
Ask Dr. Bob: Why do we hear both terms “wind” and “winds”? Isn’t wind singular, as in “wind is out of the southwest” instead of “winds out of the southwest”? Just a curiosity that came to me this morning.
This is a very good point; I think, like much else in English, there is no rational basis for the interchangeability of the two terms.
However, in writing, I think I follow this convention:
a) if I am speaking of the wind over a considerable period of time, i use the plural;
b) if I am referring to the current direction and velocity, I use the singular.
c) if I am using the noun preceded by either the definite or indefinite singular article followed by a singular verb, I use wind;
d) if I am using a plural article and predicate, then I use “winds.”
Thanks for this.
Do australia’s cold fronts come from antartica and are they like ours?
Yes, they do. Theirs are not as intense as ours because theirs travel over about 2,500 miles of ocean before reaching land, while ours travel all of the way over land.
Why do you use millibars as a unit of measure and barometric pressure is measured with something else?
It is the international standard; inches are only used in public NWS products; the remainder of the world (except for former Soviet countries) uses millibars, which has now been converted to hectopaschals; the former Soviet countries use millimeters, which medical products in the United States also use. Millibar is the most widely used measure, and is standard on all maps and discussion products.
I believe we’ll run snear to below normal in rainfall through about March; beyond that, the elong-range outlooks are taking us back to normal. This sounds pretty reasonable as there is no significant signature in the Equatorial Pacific. The one problem with this outlook: we do not yet fully understand the effects of a circulation called the “PDO”–Pacific Decadal Oscillation. That’s why sticking with a near normal rainfall outlook after March 2013 looks valid.
We’ll know this time next year!
Do sea breezes always blow toward beach, like in Corpus? Seems that during a cold front, breezes would blow toward water.
When it is the sea-breeze, it blows landward; when the wind blows offshore as you are referring to, it is called the land-breeze. Thus during most of the year in Texas, the land-breeze blows at night, and the sea-breeze blows during the day. This is because the land is cooler at night, while the sea is cooler during the day.
Does the wind ever get over 5 MPH at Verkhoyansk, Russia? Everytime, any season, I look at their weather, the wind is calm or 2 MPH.
Russian stations report in MPS–meters per second; to convert that into miles per hour, multiply by nine-fourths; thus, a 5 mps wind velocity would about 11 mph. All stations in the former Soviet Union and many stations in the former Soviet block still use the mps wind velocity measurement, and measure barometric pressure in millimeters of mercury as opposed to inches or millibars.
As a better answer to your question, yes I believe that it would. I tried to find the station on the locater list so I could check their coordinates–as I do not really know where it is. I could not locate the station.
My guess is that the equipment is old and is not reading correctly. It would be highly unusual for a station to have wind velocities that low.
The best way is to note the sun angle at solar noon. Solar noon here is about 1:21 p.m. CDT; the sun angle decreases by about one degree every four days. What you could do is this: place a stake in the ground where it gets full sun, and measure the length of the shadow; then four days later, come back and it will be a little longer, and it will continue to lengthen until December 21.
The sun angle above the horizon at solar noon on June 21 is atout 80 degrees; on December 21 at solar noon (12:21 p.m. then because we’re back on standard time) is about 36 degrees.
If a named storm is in the Pacific and crosses to the Gulf of Mexico will it be re-named?
Yes, it is–and it has occasionally happened.
Could you explain this statement: “The 500-mb. Height is 590 dm and rising, so the warming-up persists.”
The 500-mb (millibar) height refers to the oint in the atmosphere at which the air pressure falls to 500 millibars–about 15.00 inches of mercury; the mean height for that is about 18,000 feet (about 5,500 meters or 550 dm–decameters.) If the height is greater, than it is hotter here because as air flows downward, it warms. Thus, 590 decameters is about 19,000 feet. This means upper air high pressure, downward-moving air (subsidence), and hot temperatures on the surface. During the intense heat of last Summer, the 500-mb. level was about 610 dm.
We use decameters instead of feet for the 500-millibar level because it is a smaller number, and the remainder of the world uses the metric system.
In reference to your earlier response regarding thinning of the Arctic sea ice, what are your opinions on the weather effects it will have? Specifically to satisfy my curiosities, I’m interested if it will result in higher year round temps or just higher winter temps, year round precipitation, and the seasons(longer or shorter seasons, early or late seasons).
Here is my best answer:
a) I believe we will have higher precipitation; in fact, we use something called a “standard climate” in referring to normal. They are thirty-year averages, and are re-calculated every ten years. We’re currently using the 1981-2010 standard climate. When I started in the weather business, we were using the 1931-1960; our yearly average rainfall has laready increased by about two inches.
b) I think it will be more a matter of temperature extremes along with a slow rise in temperature. I’m a bit reticent to make temperature comparisons using the standard climate for Tyler since we have significantly urbanized since the climate I started with.
Beyond that, I don’t think I know enough to say anything with any degree of certainty.
I’m confused about the tropical storm names this season. We had Alberto, then Hurricane Bud. Now we have Tropical Storm Beryl. Where did Bud fit in? I thought we went straight through the alphabet?!
Different oceans: in 2012, the Atlantic names begin with a masculine name (Alberto), then Beryl; the Eastern Pacific names begin with a feminine name (Aletta), and then Bud.
What is your forecast for the summer of 2012? Is this summer looking like a repeat of summer 2011 as far as temperatures and rainfall? It would be nice if we could just have a normal summer with average rainfall and temperatures.
I do not believe this Summer will be as hot nor as dry as was last Summer. My reasoning: the LaNina period in the East Central Equatorial Pacific has broken down. That would suggest normal rainfall. The continued presence of dry soils over much of this part of the country suggests that temperatures will run somewhat above normal–but nothing like what we had last Summer.
The two weaknesses in my assumptions:
a) There is another circulation pattern called the Pacific Decadal Oscillation–a massive upper air pattern which covers much of the Northern Hemispheric Pacific Ocean. We don’t fully understand that yet; and
b) The models are not yet taking into account decreased Arctic Ocean sea ice caused by the global warming–which is a fact.
Still, I think precipitation between now and late-August should run between 7.0 and 10.0 inches; we will have some 100-plus days–but nothing like the fifty-eight we had last year.
Statewide: West Texas will likely continue in drought with easing later in
the year; East Texas: I expect near to above normal precipitation at least for the next two or three months–and probably beyond.
The forecasting models have not done well since December on precipitation in our part of the state. LaNina persisted until the middle of last month, which would have suggested below normal rainfall. Instead, we have had about 150 percent of normal precipitation since December 1.
NWS thinks the problem they are having with the models is not having factored in reduction in Arctic ice due to global warming.
The observations for climate purposes (Tyler–City) are taken at my house on the south side. They are manual, and not automated.
a) Mean winter precipitation has been about 15 percent above normal;
December was quite wet, January near normal, and February below normal (thus
far); that for February is about to change;
b) We are emerging from LaNina; NWS thinks it will be early May before the signature completely goes away; however, one encouraging sign is that warm water is downwelling in the Central Equatorial Pacific. That means that sea-surface temperatures and ocean heat content will be rising; that, in
turn, means that we’ll have more Pacific moisture above 8,000 feet to perhaps bring us better rains than last warm season.
You mentioned transitioning to a Spring pattern next month. Would you briefly expand on that situation.
Though it sounds early–it actually is not; the transition occurs because of greater sunlight and a higher sun angle; this precedes substantial surface warming by a few weeks–just as transitioning into a Fall pattern starts in mid-August–before we notice much change down here on the ground. The reason for the delay: the slowness of ground to respond with higher
temperatures to incresed sunlight, and vice-versa for the Fall transition. We call that characteristic “specific heat”.
Do you feel like the LaNina front is coming back or are just on the tail end as it moves out.
Yes, I do believe we will have a weak to moderate LaNina this Winter–not as significant as last Winter. This would suggest near normal temperatures with below normal rainfall.
Do fall and winter hold any good news for rain in the East TX and DFW area?
You’re not going to like this. It appears as if precipitation will continue at or below normal well into the cool season. We’re going to be better off than we have been, but we’re not going to be making up our deficits. LaNina, though in weakened form, is forecast to persist. A new science called “dendrochronology”–determining previous weather conditions from tree-ring data, says that protracted dry periods have occurred in the past. We can trace our climate averages back to 1426. Our current dry period is comparable with that of 949-1956. That we have observations for. Prior to that, we go back to 1716-1725, and then 1450-1489. This is probably very much more than you wanted to know, but I’ve been reading about it lately and wanted to tell somebody.
There actually is some hope; the upper air high should go east of us late this week, giving us some rain–perhaps. If we get some rain, then we will cool for a few days. Also, I agree with you–I’ve had more than enough of it. Insofar as the entire month, the models are keeping our temperatures above normal. We’ll see.
A bit of a correction. Hurricanes (Atlantic, Eastern Pacific, and Central Pacific Basin), typhoons (Western Pacific Basin) and cyclones
(Indian Ocean Basin) all rotate counter-clockwise in the Northern Hemisphere–and so do tornadoes. In the Southern Hemisphere, the rotation of all is clockwise. This is because of something called the Coriolis force.
Do you have any idea when we might get some relief from the nearly non-stop winds of the last few months? This is the windiest late winter and spring I can recall. It’s nearly June now. Surely this will stop some time…won’t it? I’m a fisherman, and every trip to the lake is a beating.
These winds are caused by storm systems migrating in slowly form the Pacific Coast, and then traversing the Plains very slowly; by the time they have reached the Mid-West, there is another on the Pacific Coast; after a day or two of respite, the process starts all over again.
Climatologically, they should let up in early June. By that time, the procession of storms across the Pacific has shifted well north of the United States. I see no reason to think that this will not happen this year, as well.
What has been the main driving force behind these cool fronts not making it this far south?..Here in south La. we’ve had consistant southerlies for the past 6 to 8 weeks that have been 6 to 12 mph higher than normal. I know this southerly wind flow has been feeding the midwest storms as they come through. Normally we get about 50% of these frontal boundaries through our area. We depend so much for spring rains around here. Summer rains normally come from tropical systems.
A strong upper air high pressure ridge, centered over South Mexico. This may be the result of the La Nina event of the past Winter. That event is winding down, and rainfall should return to normal at mid-Summer.
Weakening LaNina events tend to produce an active hurricane season in the Atlantic Basin. Attempting to accurately predict a landfall is a bit speculative.
Dr. Peters, following up on our December email exchange below and noting that your recent forecasts and comments seem to be a little more optimistic about rain, do you in fact see a change coming? If so, do you see a return to “normal” spring rains in time to get some water before going into the summer? I appreciate your good work and all details are also appreciated.
Unfortunately, our cool season forecast on precipitation was correct; on temperature, it was not; we did not go into a typical La Nina Winter until mid-February; we were there for much of December.
Now, for the Spring and Summer.
SST (sea-surface temperature) anomalies have weakened in the past few weeks, meaning that temperatures are back to near normal values in the far Eastern Pacific, and about 1.0C below normal in the Central Equatorial Pacific. In addition, ocean heat content is improving, with the below normal heat content now down to only about 150-200M. This suggests that the LaNina event is weakening, and will likely dissipate in a couple of months.
For us, this suggests continuing below normal monthly averages through mid-Summer, with improving averages at late-Summer. This said, there appers to be a short-term reprieve coming.
The storm track, which has been along about 45N for the past five or six weeks, is getting shoved back southward–at least for next week. In other words, I think we’ll see some rainfall Sunday/Monday, and perhaps again towards late-week.
P.S.: I wish I had been wrong about the cool season forecast.
The answer is that it goes both ways. A narrow channel of negatively-charged particles drops from the cloud–which we cannot see; positively charged particles then travel back to the cloud through the negative channel. This is what we see.
I have pasted below the page from the National Severe Storms Laboratory which has much more information.
What is lightning?
Lightning, as best we understand, is a channel of negative charge, called a stepped leader that zigzags downward in roughly 50-yard segments in a forked pattern. This step leader is invisible to the human eye, and shoots to the ground in less time than it takes to blink. As it nears the ground, the negatively charged step leader is attracted to a channel of positive charge reaching up, a streamer, normally through something tall, such as a tree, house, or telephone pole. When the oppositely-charged leader and streamer connect, a powerful electrical current begins flowing. A return stroke of bright luminosity travels about 60,000 miles per second back towards the cloud. A flash consists of one or perhaps as many as 20 return strokes. We see flicker when the process rapidly repeats itself several times along the same path. The actual diameter of a lightning channel is one-to-two inches.
What causes lightning to be colored rather than the usual white or blue?
Lightning can appear to be many different colors depending on what the light travels through to get to your eyes. In snowstorms, where is somewhat rare, pink and green are often described as colors of lightning. Haze, dust, moisture, raindrops and any other particles in the atmosphere will affect the color by absorbing or diffracting a portion of the white light of lightning.
Why are positive lightning bolts deemed more dangerous than the more common negatively charged bolts?
Positive lightning is often considered more dangerous because its electrical field is stronger (forming at the top of the storm), the flash duration is typically longer, and its peak charge can be much greater than a negative strike. Plus, positively charged lightning can occur near the edge of a cloud or strike more than 10 miles away – when people aren’t aware of the danger.
What are cloud flashes?
A cloud flash is lightning that occurs inside the cloud, travels from one part of a cloud to another, or from the cloud to the air.
Does lightning strike from the sky down, or the ground up?
The answer is both. Cloud-to-ground lightning comes from the sky down, but the part you see comes from the ground up. A typical cloud-to-ground flash lowers a path of negative electricity (that we cannot see) towards the ground in a series of spurts. Objects on the ground generally have a positive charge. Since opposites attract, an upward streamer is sent out from the object about to be struck. When these two paths meet, a return stroke zips back up to the sky. It is the return stroke that produces the visible flash, but it all happens so fast – in about one-millionth of a second – so the human eye doesn’t see the actual formation of the stroke.
How does the Earth benefit from lightning?
The earth benefits from lightning in several ways. First, lightning helps the Earth maintain electrical balance. The Earth is recharged by thunderstorms. The Earth’s surface and the atmosphere conduct electricity easily-the Earth is charged negatively and the atmosphere, positively. There is always a steady current of electrons flowing upwards from the entire surface of the Earth. Thunderstorms help transfer the negative charges back to Earth (lightning is generally negatively charged). Without thunderstorms and lightning, the earth-atmosphere electrical balance would disappear in 5 minutes. Lightning also produces ozone, a gas that helps protect the Earth from the dangerous rays of the sun.
How many people are killed by lightning?
According to the National Weather Service, during the past 30 years (1979-2008) lightning killed an average of 58 people each year. Documented injuries average about 300 per year, although undocumented injuries are likely to be much higher.
What happens to the ground when lightning strikes it?
What tends to happen when lightning strikes ground is that it fuses dirt and clays in to silicas. The result is often a black, glassy rock (called a fulgarite) in the shape of a convoluted tube. The shape in the ground is the shape of the path the lightning current followed in the ground. There is often damage to grasses along this path too. Lightning traveling down a tree trunk turns water to steam. If it gets under the bark into the surface moisture of the wood, the rapidly expanding steam can blast pieces of bark from the tree, and the wood along the path is often killed.
Can lightning strike the same place twice?
Lightning does hit the same spot (or almost the same spot) more than once, contrary to folk wisdom. It could be simply a statistical fluke (i.e., with all the lightning that occurs, eventually lightning will strike somewhere near a previous lightning strike within a short period of time). It could also be that something about the site makes it somewhat more likely to be struck. Typically, when lightning strikes something on the ground, the object that is struck sends a faint channel upward that joins the downward developing flash and creates the connection to the ground. Taller objects are more likely than shorter objects to produce the upward channel. But it is also possible that something that locally affects the ability of the ground to conduct electricity (such as the salt or moisture content of the ground at the time, the presence or absence of rock, standing water, pipes or other metal objects in the ground), the terrain shape, the shape of leaves or twigs, or something else might make a particular location more likely than another nearby location to be struck.
What is a “stepped leader?”
A stepped leader is a stream of weakly charged particles that flows from the cloud – it moves towards the ground, starting and stopping, and sometimes branching, trying to find the path of least resistance.
Is it possible to have lightning without thunder?
No, it is not possible to have lightning without thunder. Thunder is a direct result of lightning. However, it IS possible that you could not hear the thunder because it was too far away. Sometimes it is called “heat lightning” because it occurs most often in the summer.
What is it called when lightning strikes sand and melts it, forming a tube?
Fulgarite. Fulgarite has been found all over the world, but is relatively rare. The color depends on the minerals in the sand that was struck.
Is lightning always produced by a thunderstorm?
Yes, lightning is always produced by a thunderstorm. Lightning causes thunder, and you can’;t have a thunderstorm without thunder. Thunderstorms are the only weather condition strong enough to carry water droplets to the upper parts of the atmosphere where they will freeze and become charged – because thunderstorms have an updraft.
Does lightning always strike the tallest object?
Never say always! Lightning USUALLY strikes the tallest object. It makes sense that the tallest object is most attractive, because it is the easiest path for the lightning to take.
NOAA safety posters say lightning can strike 10 miles away from a thunderstorm. Is this true?
Yes, it is true. Lightning that strikes away from a thunderstorm are often called “bolts from the blue.” Lightning has its own agenda. It is random and unpredictable, and defies our attempts to fit it into a convenient box to describe its behavior. We don’t really know why it sometimes connects with the ground and not a tree, or a beach instead of the water. Check out these photos:
c.. http://www.srh.noaa.gov/mlb/BBX.html shows a radar section with lightning data overlayed (white dots). See the white dots extending out from the core of the storm to the right – about 17km away from the back of the storm?
A helmeted bicyclist experienced a lightning strike to the head under fair weather conditions with a cloudless sky. It was determined that the bolt probably originated in a thunderstorm that was about 16km away and obscured by mountains.
Lightning strikes the ground approximately 25 million times each year in the U.S. According to the NWS, the chance of an individual in the U.S. being killed or injured during a given year is one in 240,000. Assuming an average life span of 80 years, a person’s odds over their lifetime becomes one in 3000. Assuming the average person has ten family members and others with whom they are close, then the chances are one in 300 that a lightning strike will closely affect a person during their lifetime.
What type of electricity is lightning?
Lightning is an electrostatic discharge accompanied by the emission of visible light and other forms of electromagnetic radiation.
How many volts and watts are in lightning?
Lightning can have 100 million to 1 billion volts, and contains billions of watts.
How hot can lightning make the air?
Energy from lightning heats the air anywhere from 18,000 degrees Fahrenheit to up to 60,000 degrees Fahrenheit.
How many lightning deaths are water-related?
In a study of 35 years of lightning incident statistics, 8% were water-related.
Can lightning kill fish?
Lightning striking the water can penetrate down and kill fish nearby.
Where can I get information on lightning strikes that occur in my area?
NSSL does not archive lightning data, but there are several other companies that do. We actually purchase lightning data ourselves (we do not have the funds to maintain our own network) and have strict rules about how we can use it.
What is dry lightning?
Dry lightning is lightning that occurs without rain nearby. The NOAA Storm Prediction Center routinely forecasts dry lightning because this kind is more likely to cause forest fires.
What causes thunder?
Thunder is caused by lightning. The bright light of the lightning flash caused by the return stroke mentioned above represents a great deal of energy. This energy heats the air in the channel to above 50,000 degrees F in only a few millionths of a second! The air that is now heated to such a high temperature had no time to expand, so it is now at a very high pressure. The high pressure air then expands outward into the surrounding air compressing it and causing a disturbance that propagates in all directions away from the stroke. The disturbance is a shock wave for the first 10 yards, after which it becomes an ordinary sound wave, or thunder. Thunder can seem like it goes on and on because each point along the channel produces a shock wave and sound wave.
How long can a lightning bolt be?
Recent research from Vaisala-GAI’s LDAR and LDAR II lightning detection networks show that lightning can travel 60 miles or more. The longest bolts start at the front of a squall line and travel horizontally back into clouds trailing behind the squall line. The longest bolt they have seen to date was 118 miles long in the Dallas-Ft. Worth, TX area. Since 3-D lightning measurements are relatively new, scientists are learning more every day and these numbers may change.
Where does lightning usually strike?
Lightning comes from a parent cumulonimbus cloud. These thunderstorm clouds are formed wherever there is enough upward motion, instability in the vertical, and moisture to produce a deep cloud that reaches up to levels somewhat colder than freezing.
These conditions are most often met in summer. In general, the US mainland has a decreasing amount of lightning toward the northwest. Over the entire year, the highest frequency of cloud-to-ground lightning is in Florida between Tampa and Orlando. This is due to the presence, on many days during the year, of a large moisture content in the atmosphere at low levels (below 5,000 feet), as well as high surface temperatures that produce strong sea breezes along the Florida coasts. The western mountains of the US also produce strong upward motions and contribute to frequent cloud-to-ground lightning. There are also high frequencies along the Gulf of Mexico coast westward to Texas, the Atlantic coast in the southeast US, and inland from the Gulf. Regions along the Pacific west coast have the least cloud-to-ground lightning.
Does lightning happen during the winter?
Lightning occurs less frequently in the winter because there is not as much instability and moisture in the atmosphere as there is in the summer. These two ingredients work together to make convective storms that can produce lightning. Without instability and moisture, strong thunderstorms are unlikely.
During the winter, the land surface is cooler because there is not as much heating by the sun to warm it up. Without warm surface temperatures, the near-surface air wouldn’t rise in the atmosphere very far. Thus, the kinds of deep (8-15 km deep) thunderstorms that develop in the summertime wouldn’t develop.
Warm air holds more water vapor. And, when water vapor condenses into liquid water cloud drops, latent heat is released which fuels the thunderstorm. So, warm, moist air near the surface (and the proper conditions aloft to give you lots of instability) can result in deep convection, which may produce lightning discharges.
Clouds become electrified when strong updrafts (fueled by the instability and moisture) bring supercooled liquid water drops and ice crystals at temperatures less than freezing (0 deg C) together. In this environment, interactions between the ice crystals and supercooled water droplets produce electric charges. The exact mechanisms by which this charging happens remain unknown. The electrical charges build up until they are strong enough to overcome the resistance of the surrounding air. The breakdown of the electric fields produced by these charges is the lightning bolt.
What is thundersnow?
Although thunderstorms are less common in the winter, sometimes lightning can occur within snowstorms. Called thundersnow, relatively strong instability and abundant moisture may be found above the surface, such as above a warm front, rather than at the surface where it may be below freezing. Thundersnow is sometimes observed downstream of the Great Salt Lake and the Great Lakes during lake-effect snowstorms, too.
What is a “bolt from the blue”?
A “Bolt from the Blue” is a cloud-to-ground flash which typically comes out of the back side of the thunderstorm cloud, travels a relatively large distance in clear air away from the storm cloud, and then angles down and strikes the ground. These lightning flashes have been documented to travel more than 25 miles away from the thunderstorm cloud. They can be especially dangerous because they appear to come from clear blue sky.
Can lightning be detected?
Since the 1980s, cloud-to-ground lightning flashes have been detected and mapped in real time across the entire US by several networks. In 1994, the networks were combined into one national network consisting of antennas that detect the angle from ground strike points to an antenna (direction-finder antenna), that detect the time it took for them to arrive at an antenna (time-of-arrival method), or a combination of both detection methods.
Flashes have also been detected from space during the past few years by an optical sensor . This experimental satellite covers the earth twice a day in tropical regions. The satellite also detects flashes that do not strike the ground, but cannot tell the difference between ground strikes and cloud flashes.
How many flashes a year are there?
Over the continental 48 states, an average of 20,000,000 cloud-to-ground flashes have been detected every year since the lightning detection network covered all of the continental US in 1989. In addition, about half of all flashes have more than one ground strike point, so at least 30 million points on the ground are struck on the average each year in the US. Besides cloud-to-ground flashes, there are roughly 5 to 10 times as many cloud flashes as there are ground flashes.
What types of damage can lightning cause?
Cloud-to-ground lightning can kill or injure people by direct or indirect means. The lightning current can branch off to a person from a tree, fence, pole, or other tall object. It is not known if all people are killed who are directly struck by the flash itself. In addition, flashes may conduct their current through the ground to a person after the flash strikes a nearby tree, antenna, or other tall object. The current also may travel through power or telephone lines, or plumbing pipes to a person who is in contact with an electric appliance, telephone, or plumbing fixture.
Similarly, objects can be directly struck and this impact may result in an explosion, burn, or total destruction. Or, the damage may be indirect when the current passes through or near it. Sometimes, current may enter a building and transfer through wires or plumbing and damage everything in its path. Similarly, in urban areas, it may strike a pole or tree and the current then travels to several nearby houses and other structures and enter them through wiring or plumbing.
How can I stay safe from lightning?
NOAA’s National Weather Service is an excellent source for information on indoor and outdoor lightning safety and lightning risks.
What are the odds of being struck by lightning?
The odds of being struck in your lifetime (estimated to be 80 years) are 1 in 3000.
In the case of high clouds (cirrus), they are bands of moisture pushed along by higher velocity winds. Low clouds (stratus) are less likely to do that, but occasionally do. In actuality, the cirrus clouds are ice crystals.
What has been the main reason for the winter storms this year during a La Nina? My best guess is the jet stream has dipped further south than expected. I’d like to read about your thoughts.
Two things have come together. First, the Pacific-North American Tele-Connection (the flow of air from Siberia across the North Pacific and into North America) has been oriented from northwest to southeast; second, the Arctic Oscillation (the flow of air from the Arctic region) has been oriented northeast to southwest. Thus, very cold air has been funneled southward.
That is the simple part of the answer. The more complex part for which I have read no satisfactory answer, is why.
ANSWER: – The dryness this Winter is the result of La Nina–the opposite of El Nino; this means cool waters in the East Central Equatorial Pacific Ocean. The dry conditions look to continue well into 2011.
Dr. Bob, I have followed your forecasts and comments for years and appreciate your good work. My question: I understood that last year was a typical El Nino winter and someone said following that we would have a dry summer and fall. That has been very correct and I am wondering if we follow the “normal” patterns, when would the rains return? Not an official forecast but just what is the normal coming off the El Nino? I live between W’house and Troup and we are probably 7 or 8 inches below Tyler which is not so good itself. Thank you for your time.
This won’t be encouraging; the SST (sea-surface temperatures) and low ocean heat content (down to 300M) are quite certainly in a La Nina phase in the East Central Equatorial Pacific; those values are forecast to continue at present levels for several months, yet. I’d think it will probably be some time well into 2011 before we start getting significant rainfall again.