Hawaiian Islands weather details & Aloha paragraphs / September 14-15, 2008

September 14-15 2008

Air Temperatures – The following maximum temperatures were recorded across the state of Hawaii Sunday afternoon: 

Lihue, Kauai – 83
Honolulu, Oahu – 86
Kaneohe, Oahu – 84
Kahului, Maui – 87
Hilo, Hawaii – 86
Kailua-kona – 85

Air Temperatures ranged between these warmest and coolest spots near sea level, and on the taller mountains…at 3 p.m. Sunday afternoon:

Kahului, Maui – 87F  
Lihue, Kauai – 80

Haleakala Crater- missing (near 10,000 feet on Maui)
Mauna Kea summit – 45 (near 14,000 feet on the Big Island)

Precipitation Totals – The following numbers represent the largest precipitation totals (inches) during the last 24 hours on each of the major islands, as of Sunday afternoon:

0.55 Mohihi Crossing, Kauai
1.01 Waiawa, Oahu
0.00 Molokai
0.00 Lanai
0.00 Kahoolawe
0.32 Kaupo Gap, Maui
0.12 Waiakea Uka, Big Island

Weather Chart – Here’s the latest (automatically updated) weather map showing a 1026 millibar high pressure system located far to the northeast of Hawaii…with its associated ridge, now located just north of Kauai…gradually moving northward.  This pressure configuration will keep our winds light Monday morning…slowly strengthening into Tuesday.

Satellite and Radar Images: To view the cloud conditions we have here in Hawaii, please use the following satellite links, starting off with the Infrared Satellite Image of the islands to see all the clouds around the state during the day and night. This next image is one that gives close images of the islands only during the daytime hours, and is referred to as a Close-up visible image. This next image shows a larger view of the Pacific…giving perspective to the wider ranging cloud patterns in the Pacific Ocean. To help you keep track of where any showers may be around the islands, here’s the latest animated radar image. 

Hawaii’s Mountains – Here’s a link to the live webcam on the summit of near 14,000 foot Mauna Kea on the Big Island of Hawaii. The tallest peak on the island of Maui is the Haleakala Crater, which is near 10,000 feet in elevation. These two webcams are available during the daylight hours here in the islands…and when there’s a big moon rising just after sunset for an hour or two! Plus, during the nights and early mornings you will be able to see stars, and the sunrise too…depending upon weather conditions.

Aloha Paragraphs

  Tonight is the September full moon
Photo Credit: flickr.com

Our winds will remain light and variable Sunday…with a tendency towards southeast. These light SE breezes have carried lots volcanic haze up over the islands, from the vents on the Big Island. Sunday will have poor air visibilities, with some of the thickest vog that we’ve seen since the late spring months. The return of trade winds Monday will begin the process of clearing our local atmosphere, but it will likely take until Tuesday before we see greatly improved air quality. The trade winds will continue blowing through the rest of the new week.

The emphasis for showers will be focused over the upcountry interior sections, especially over and around the leeward slopes. A trough of low pressure aloft, which has destabilized our local atmosphere some, especially over Kauai and Oahu…will move away soon. Nonetheless, we will find clouds gathering over and around the mountains on all the islands Sunday afternoon, with some showers falling locally. As the trade winds return soon, the bias for showers will slip back over to the windward sides.

It’s early Sunday afternoon here in Kula, Maui, as I begin writing this last paragraph of today’s tropical weather narrative from Hawaii.  Clouds gathered around the mountains Sunday afternoon, with showers falling here and there, at least here in Kula…as I type these words. The beaches have remained mostly sunny, warm, and quite humid. The only place that finds the trade winds blowing at the moment, or at least with any strength…was down at South Point on the Big Island. As you saw in the picture as you were scrolling down the page, tonight is the full moon. This big moon reaches its fullest aspect, here in the islands, at 11:14 p.m. This moon may have a slight muted color to it, as has the sun going down, through the volanic haze the last couple of evenings. At 3pm Sunday afternoon, it was 87F degrees in Kahului, and at the same time, a thick and foggy 66F degrees here in Kula…at the 3,100 foot elevation. It’s an interesting life we’re living now…isn’t it!  I’ll be back very early Monday morning with your next new weather narrative. I hope you have a great Sunday night until then! Aloha for now…Glenn.

Interesting:

Cutting down on the use of paper is easy enough, but in spite of all your efforts you’ll never become 100% paperless. That’s where tree free paper comes in. Recently launched on the market by GPA, a Chicago paper company, Ultra Green paper is 100% tree free. And of equal importance; the paper is produced without any water. What more can you ask for? This paper is going to be a massive selling point for business leaders vying for deals. Not to speak of green design/advertising. Ultra Green is made from inorganic mineral powders derived from limestone and calcium carbonate, with a trace amount of non-toxic resin and high density polyethylene (HDPE) as a binding agent. No chlorine is used. Sounds too good to be true? There’s more! Ultra Green paper is also won’t yellow or become brittle no matter how long it’s exposed to sunlight. The paper is resistant to scuffing, water, grease and oils and can be used outdoors without being at risk from decomposing.

Plus it offers antimicrobial protection and conforms to FDA standards for food contact! And due to the water and energy savings made in its manufacturing process, Ultra Green paper is priced 30 to 40% below than regular synthetic paper and film. Replacing one ton of traditional paper with one ton of Ultra Green paper saves 20 trees, according to Environmental Defense’s paper calculator. It also eliminates 42 lbs of waterborne waste, 7,480 gallons water/wastewater, 167 lbs solid waste and 236 lbs carbon emissions. Energy savings amount to 25 million BTU. GPA says that the paper combines the printability of a traditional paper product with the durability of a plastic sheet. It does not require special inks or manufacturing processes. This paper ought to be the invention of the year!

Interesting2:

The amount of sea ice around Antarctica has grown in recent Septembers in what could be an unusual side-effect of global warming, experts said on Friday. In the southern hemisphere winter, when emperor penguins huddle together against the biting cold, ice on the sea around Antarctica has been increasing since the late 1970s, perhaps because climate change means shifts in winds, sea currents or snowfall. At the other end of the planet, Arctic sea ice is now close to matching a September 2007 record low at the tail end of the northern summer in a threat to the hunting lifestyles of indigenous peoples and creatures such as polar bears. "The Antarctic wintertime ice extent increased…at a rate of 0.6 percent per decade" from 1979-2006, said Donald Cavalieri, a senior research scientist at the NASA Goddard Space Flight Center. At 19 million sq kms (7.34 million sq mile), it is still slightly below records from the early 1970s of 20 million, he said. The average year-round ice extent has risen too. Some climate skeptics point to the differing trends at the poles as a sign that worries about climate change are exaggerated. However, experts say they can explain the development.

"What’s happening is not unexpected…Climate modelers predicted a long time ago that the Arctic would warm fastest and the Antarctic would be stable for a long time," said Ted Maksym, a sea ice specialist at the British Antarctic Survey. The U.N. Climate Panel says it is at least 90 percent sure that people are stoking global warming — mainly by burning fossil fuels. But it says each region will react differently. A key difference is that Arctic ice floats on an ocean and is warmed by shifting currents and winds from the south. By contrast, Antarctica is an isolated continent bigger than the United States that creates its own deep freeze. "The air temperature in Antarctica has increased very little compared to the Arctic," said Ola Johannessen, director of the Nansen Environmental and RemoteSensingCenter in Norway. "The reason is you have a huge ocean surrounding the land." Cavalieri said some computer models indicate a reduction in the amount of heat coming up from the ocean around Antarctica as one possible explanation for growing ice. Another theory was that warmer air absorbs more moisture and means more snow and rainfall, he said. That could mean more fresh water at the sea surface around Antarctica — fresh water freezes at a higher temperature than salt water.

Interesting3:

The first whales once swam the seas by wiggling large hind feet, research now suggests. These new findings shed light on the mysterious shift these leviathans made away from land. The ancestors of whales once strode on land on four legs, just as other mammals do. Over time, as they evolved to dwell in water, their front legs became flippers while they lost their back legs and hips, although modern whales all still retain traces of pelvises, and occasionally throwbacks are born with vestiges of hind limbs. A great deal of mystery surrounds how the anatomy of the first whales changed to propel them through the water. A key piece of that puzzle would be the discovery of when exactly the wide flukes on their powerful tails arose. "The origin of flukes is one of the last steps in the transition from land to sea," explained vertebrate paleontologist Mark Uhen of the Alabama Museum of Natural History in Tuscaloosa.  To shed light on this mystery, Uhen analyzed new fossils that amateur bone hunters discovered exposed along riverbanks in Alabama and Mississippi.

These bones once belonged to the ancient whale Georgiacetus, which swam along the Gulf Coast of North America roughly 40 million years ago, back when Florida was mostly submerged underwater. This creature reached some 12 feet in length and likely used its sharp teeth to dine on squid and fish.  The first whales known to possess flukes are close relatives of Georgiacetus that date back to 38 million years ago. But while only about 2 million years separate Georgiacetus from these other whales, Uhen now finds that Georgiacetus apparently did not possess flukes. The new 2-inch-long tail vertebra he analyzed — one of some 20 tail vertebrae the ancient whale had — is not flattened as the vertebrae near whales flukes are.  Instead, Uhen suggests that Georgiacetus wiggled large back feet like paddles in order to swim. Past research showed this ancient whale had large hips, which suggested it also had large hind legs. Oddly, scientists had also found that its pelvis was not attached to its spine. This meant its hind legs could not paddle in the water or support the whale’s body weight on land, leaving it a puzzle as to what they were for until now.

Interesting4: As Hurricane Ike pummels the Texas coast, the only thing standing in the way is a thin stretch of land called Galveston. Galveston is a barrier island, a narrow landmass made mostly of sand that extends along a coastline parallel to the land. These islands, common along the Gulf Coast and East Coast of the United States, are some of the most fragile and changing landforms on Earth. And they are particularly vulnerable to storms. "Barrier islands are exposed to the open ocean, and the waves and storm surges generated by hurricanes," said Bob Morton, a geologist at the U.S. Geological Survey’s Center for Coastal and Watershed Studies in St. Petersburg, Fla. "As a storm makes landfall they’re the ones that are going to receive the strongest winds and the highest wave actions." National Hurricane Center officials have warned residents of Galveston to evacuate or else face "certain death," though several thousand are thought to be staying put.

Barrier islands like Galveston are particularly vulnerable to storm damage because they are made of sand, as opposed to the hard bedrock that underlies larger islands and the mainland. They also tend to have very low elevations, making it easy for water to wash over and submerge the island. Many have questioned the wisdom of choosing to build on and develop barrier islands, given their risks. "Every year there’s reporting on the foolishness of building on barrier islands, but people are going to do it anyway," Morton told LiveScience. "We don’t learn from the past. If you look at the barrier islands on the Mississippi coast in particular, after both Hurricane Camille in 1969, and Katrina, what did they do? They rebuilt. It’s a perfect example of a coastal area that did get hit as bad as it can get, and they just go back and rebuild."