Wednesday Wonderment – Ep. 29

From both sides now…

This week, I’m reaching to the skies for an additional source of wonderment.  It’s not the beautiful shades of blue that are the result of Rayleigh Scattering in the upper atmosphere, but rather the window dressing above our pates that changes on a regular basis: Clouds.

Clouds are a never-ceasing source of inspiration, meditation and contemplation.  They can hide the Sun, or provide a source for daydreams, as we imagine what the shapes of each of the clouds are.  They can be heavy and dense, threatening with inclement weather, or light and whispy, letting us know that the weather is just perfect!

Here’s a view of streaky clouds blowing across the sky…

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Sunrise Streaks

The origin of the term cloud can be found in the old English clud or clod, meaning a hill or a mass of rock. Around the beginning of the 13th century, it was extended as a metaphor to include rain clouds as masses of evaporated water in the sky because of the similarity in appearance between a mass of rock and a cumulus heap cloud. Over time, the metaphoric term replaced the original old English weolcan to refer to clouds in general.

History of cloud science and nomenclature

Aristotle and Theophrastus

Ancient cloud studies were not made in isolation, but were observed in combination with other weather elements and even other natural sciences. In about 340 BC the Greek philosopher Aristotle wrote Meteorologica, a work which represented the sum of knowledge of the time about natural science, including weather and climate. For the first time, precipitation and the clouds from which precipitation fell were called meteors, which originate from the Greek word meteoros, meaning ‘high in the sky’. From that word came the modern term meteorology, the study of clouds and weather. Meteorologica was based on intuition and simple observation, but not on what is now considered the scientific method. Nevertheless, it was the first known work that attempted to treat a broad range of meteorological topics.

The magazine De Mundo (attributed to Pseudo-Aristotle) noted:

Cloud is a vaporous mass, concentrated and producing water. Rain is produced from the compression of a closely condensed cloud, varying according to the pressure exerted on the cloud; when the pressure is slight it scatters gentle drops; when it is great it produces a more violent fall, and we call this a shower, being heavier than ordinary rain, and forming continuous masses of water falling over earth. Snow is produced by the breaking up of condensed clouds, the cleavage taking place before the change into water; it is the process of cleavage which causes its resemblance to foam and its intense whiteness, while the cause of its coldness is the congelation of the moisture in it before it is dispersed or rarefied. When snow is violent and falls heavily we call it a blizzard. Hail is produced when snow becomes densified and acquires impetus for a swifter fall from its close mass; the weight becomes greater and the fall more violent in proportion to the size of the broken fragments of cloud. Such then are the phenomena which occur as the result of moist exhalation.

Several years after Aristotle’s book, his pupil Theophrastus put together a book on weather forecasting called The Book of Signs. Various indicators such as solar and lunar halos formed by high clouds were presented as ways to forecast the weather. The combined works of Aristotle and Theophrastus had such authority they became the main influence in the study of clouds, weather and weather forecasting for nearly 2000 years.

Luke Howard, Jean-Baptiste Lamarck, and the first comprehensive classification

After centuries of speculative theories about the formation and behavior of clouds, the first truly scientific studies were undertaken by Luke Howard in England and Jean-Baptiste Lamarck in France. Howard was a methodical observer with a strong grounding in the Latin language and used his background to classify the various tropospheric cloud types during 1802. He believed that the changing cloud forms in the sky could unlock the key to weather forecasting. Lamarck had worked independently on cloud classification the same year and had come up with a different naming scheme that failed to make an impression even in his home country of France because it used unusual French names for cloud types. His system of nomenclature included twelve categories of clouds, with such names as (translated from French) hazy clouds, dappled clouds and broom-like clouds. By contrast, Howard used universally accepted Latin, which caught on quickly after it was published in 1803. As a sign of the popularity of the naming scheme, the German dramatist and poet Johann Wolfgang von Goethe composed four poems about clouds, dedicating them to Howard. An elaboration of Howard’s system was eventually formally adopted by the International Meteorological Conference in 1891.

Howard’s original system established three general cloud forms based on physical appearance and process of formation: cirriform (mainly detached and wispy), cumuliform or convective (mostly detached and heaped, rolled, or rippled), and non-convective stratiform (mainly continuous layers in sheets). These were cross-classified into lower and upper étages. Cumuliform clouds forming in the lower level were given the genus name cumulus from the Latin word for heap, and low stratiform clouds the genus name stratus from the Latin word for sheet or layer. Physically similar clouds forming in the upper étage were given the genus names cirrocumulus (generally showing more limited convective activity than low level cumulus) and cirrostratus, respectively. Cirriform clouds were identified as always upper level and given the genus name cirrus from the Latin for ‘fibre’ or ‘hair’.

In addition to these individual cloud types; Howard added two names to designate cloud systems consisting of more than one form joined together or located in very close proximity. Cumulostratus described large cumulus clouds blended with stratiform layers in the lower or upper levels. The term nimbus was given to complex systems of cirriform, cumuliform, and stratiform clouds with sufficient vertical development to produce significant precipitation, and it came to be identified as a distinct nimbiform physical category.

Howard’s successors

In 1840, German meteorologist Ludwig Kaemtz added stratocumulus to Howard’s canon as a mostly detached low-étage genus of limited convection. It was defined as having cumuliform- and stratiform characteristics integrated into a single layer (in contrast to cumulostratus which was deemed to be composite in nature and could be structured into more than one layer). This led to the recognition of a stratocumuliform category that included rolled and rippled clouds classified separately from the more freely convective heaped cumuliform clouds.

During the mid 1850s, Emilien Renou, director of the Parc Saint-Maur and Montsouris observatories, began work on an elaboration of Howard’s classifications that would lead to the introduction during the 1870s of altocumulus (physically more closely related to stratocumulus than to cumulus) and altostratus. These were respectively stratocumuliform and stratiform cloud genera of a newly defined middle étage above stratocumulus and stratus but below cirrocumulus and cirrostratus.

In 1880, Philip Weilbach, secretary and librarian at the Art Academy in Copenhagen, and like Luke Howard, an amateur meteorologist, unsuccessfully proposed an alternative to Howard’s classification. However, he also proposed and had accepted by the permanent committee of the International Meteorological Organization (IMO), a forerunner of the present-day World Meteorological Organization (WMO), the designation of a new free-convective vertical or multi-étage genus type, cumulonimbus, which would be distinct from cumulus and nimbus and identifiable by its often very complex structure (frequently including a cirriform top and what are now recognized as multiple accessory clouds), and its ability to produce thunder. With this addition, a canon of ten tropospheric cloud genera was established that came to be officially and universally accepted.  Howard’s cumulostratus was not included as a distinct type, having effectively been reclassified into its component cumuliform and stratiform genus types already included in the new canon.

In 1890, Otto Jesse revealed the discovery and identification of the first clouds known to form above the troposphere. He proposed the name noctilucent which is Latin for night shining. Because of the extremely high altitudes of these clouds in what is now known to be the mesosphere, they could become illuminated by the a sun’s rays when the sky was nearly dark after sunset and before sunrise.  Three years later, Henrik Mohn revealed a similar discovery of nacreous clouds in what is now considered the stratosphere.

In 1896, the first cloud atlas sanctioned by the IMO was produced by Teisserenc de Borte based on collaborations with Hugo H. Hildebrandsson. The latter had become the first researcher to use photography for the study and classification of clouds in 1879.

Alternatives to Howard’s classification system were proposed throughout the 19th century. Heinrich Dove of Germany and Elias Loomis of the United States came up with other schemes in 1828 and 1841 respectively, but neither met with international success. Additional proposals were made by Andre Poey (1863), Clemment Ley (1894), and H.H. Clayton (1896), but their systems, like earlier alternative schemes, differed too much from Howard’s to have any success beyond the adoption of some secondary cloud types. However, Clayton’s idea to formalize the division of clouds by their physical structures into cirriform, stratiform, “flocciform” (stratocumuliform) and cumuliform (with the later addition of cumulonimbiform), eventually found favor as an aid in the analysis of satellite cloud images.

20th-century developments

A further modification of the genus classification system came when an IMC commission for the study of clouds put forward a refined and more restricted definition of the genus nimbus which was effectively reclassified as a stratiform cloud type. It was then renamed nimbostratus and published with the new name in the 1932 edition of the International Atlas of Clouds and of States of the Sky. This left cumulonimbus as the only nimbiform type as indicated by its root-name.

On April 1, 1960, the first successful weather satellite, TIROS-1 (Television Infrared Observation Satellite), was launched from Cape Canaveral, Florida by the National Aeronautics and Space Administration (NASA) with the participation of The US Army Signal Research and Development Lab, RCA, the US Weather Bureau, and the US Naval Photographic Center. During its 78-day mission, it relayed thousands of pictures showing the structure of large-scale cloud regimes, and proved that satellites could provide useful surveillance of global weather conditions from space.

In 1976, the United Kingdom Department of Industry published a modification of the international cloud classification system adapted for satellite cloud observations. It was co-sponsored by NASA and showed a change in name of the nimbiform type to cumulonimbiform, although the earlier name and original meaning pertaining to all rain clouds can still be found in some classifications.

Where to go from here…

Next time you go outside, look around you to ensure that your surroundings are safe, and then look up to the sky and take in the cloud formations that grace the firmament.  Don’t just do this once, but do it every day with appreciation for the moment, in which you find yourself.

Tuesday Photo Challenge – Round-Up 6

Cloudy is a good forecast!

Another week with fantastic entries, which were a delight to see, as it looked like you found some inspiration in this week’s topic.  In this sixth installment of the Tuesday Photo Challenge, the theme was clouds, particularly keeping in mind how they can enhance the scene that is captured in an image.

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Persistence

For those who’d like to participate in this weekly challenge, the rules are the following:

The following were this week’s participants in the challenge:

  • iballrtw of the Eyeball Around the World blog, posted a beautifully lit cloud image with sunlight streaming around the edges of the cloud.
  • Sonya of Middleton Road, posted a landscape image that together with the beautiful clouds made me feel like I was in a fairy tale.
  • Miriam of the Out an’ About blog, wove an entire story around the cloud photos that she posted, which were fantastic.
  • Nikki, who writes A Kinder Way showed some of the great Texas skies and provided interpretation to some of the great clouds in her images.
  • Debbie, of ForgivingJournal got some of her creative energy expressed through her cloud images, which inspired!
  • Steve, who writes Meandering Maverick, was stymied by a week of perfect, cloudless weather, so he regaled us with some fantastic cloud images from before.

Thank you to all of you who participated and everyone who supported by reading these posts.  Hope you had as much fun as I did!

Next Tuesday, it will be time for another topic…  I have something in mind already, that I hope will give you a bit of inspiration.

Wednesday Wonderment – pt 18

Tall and statuesque

This week appears to have been overtaken by clouds, as a central theme.  Yesterday’s Tuesday Photo Challenge is about clouds, Monday’s response to dreams included a cloud as a central character, and now today.

As I am in Israel this week and lucky enough to be staying at a hotel right at the beach, I have been able to observe some interesting cloud formations develop during the evening.  While I am certainly not an expert on clouds, the particular cloud in the image that I captured the other event made me curious enough to look for more detail.

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Clouds off the Beach

The cloud in the image is recognized by most of us as a cumulonimbus cloud, or a rain cloud, as we have seen enough of them.  What made me curious is the updrafts that were forming to create the top of this cloud, which led me to find out that there are several distinct types of cumulonimbus clouds.

Cumulonimbus calvus is a moderately tall cumulonimbus cloud which is capable of precipitation, but has not yet reached the tropopause, which is the height of stratospheric stability where it forms into a cumulonimbus capillatus (fibrous-top) or cumulonimbus incus (anvil-top). Cumulonimbus calvus clouds develop from cumulus congestus, and its further development under auspicious conditions will result in cumulonimbus incus.

This cloud consists mainly of water droplets. By definition of cumulonimbus cloud, at its top water droplets are transformed into ice crystals, but for cumulonimbus calvus content of ice crystals is small and freezing is in early stage, so cloud top still looks round and puffy.

Cumulonimbus calvus is characterized by distinctive (between other types of cumulonimbus cloud) rounded shape and relatively sharp edges of its top area, unlike cumulonimbus incus or cumulonimbus capillatus, which have cirriform tops. Developing cumulonimbus calvus loses sharp outlines of the top as more water droplets transform into ice crystals. Strong updrafts may form pileus or thin vertical stripes protruding upwards out of the cloud. When upper part of the cloud freezes to greater extent and clearly visible cirriforms appears, cumulonimbus calvus turns into another species of cumulonimbus.

Hope this was interesting to you!

Technical Details

This image was captured at the beach in Herzliya, Israel, using an iPhone 6S with the standard Camera app.

Tuesday Photo Challenge – Clouds

Clouds are for more than just storage

Welcome to the sixth installment of the Tuesday Photo Challenge!  This week’s challenge is inspired by a comment made on last week’s TPC, which made me decide to use it now. The challenge is Clouds.

This might sound like a rather straightforward challenge, but, if you have tried to get photos with clouds in them, you have probably noticed that they are not as easy to capture with a camera, as they are seen with the eye.  The reason is that the dynamic range of the eye is much broader than either film or a digital sensor.  Those beautiful fluffy clouds that we all like to admire tend to blow out your camera’s sensor, so that detail is often lost.

One way of getting around this problem is to use HDR, High Dynamic Range, imaging techniques, which are available in a lot of cameras and smartphones.  This allows you to get the cloud and the rest of your subject in a pleasing fashion.

The other part to keep in mind with this challenge is that clouds can really add to good composition, but they can also detract; as such, a photo of just clouds without any other subject may not be as compelling, as it could be with a great subject.  Also, think about lines, and how they work in your image.

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Persistence

For those who’d like to participate in this weekly challenge, the rules are the following:

  • Write a post with an image for this week’s topic
  • Please use the tag #fpj-photo-challenge (if you’re not sure about how tags work, please check out this WordPress article about tagging posts)
  • Create a pingback link to this post, so that I can create a post showing all of the submissions over the week
  • Have fun creating something new!!

I’m looking forward to seeing your creative efforts!

Technical Details

This photo was created with a Canon EOS 5D Mk II using an EF 24-105mm f/4L lens.  It was a series of 5 images with exposure values of -2, -1, 0, +1 and +2 EV with respect to the measured ‘correct’ value.  The images were processed using Photomatix Pro.