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Freitag, 03 Juni 2016 12:06

Ein kleiner Frustbeitrag zum Thema Morgennebel

Ein kleiner Frustbeitrag zum Thema Morgennebel

Seit über einer Woche bildet sich jeden Morgen eine graue Wand, die mich davon abhält die Fortsetzung zum ersten Teil des Videos über Landschaftsfotoplanung zu drehen. Ein ganz normaler Sonnenaufgang wäre schon vollkommen ausreichend, doch stattdessen hängt die Sonne jedes mal noch für Stunden hinter einem Vorhang aus Morgennebel. Aus heute war es wieder so. Ein Ärgernis, dass mich aber dazu brachte, der Sache mal theoretisch auf den Grund zu gehen! 

 

 

Natürlich habe ich das sprichwörtliche Grauen schon weit vor dem Aufgang der Sonne bemerkt. Und natürlich hätte ich mich gar nicht erst auf den Weg machen müssen, nachdem der Blick vom Balkon um 3 Uhr nachts bereits nichts gutes verhieß:

  • IMG_3001
 

Warum ich trotzdem losgezogen bin? Weil es schon seit einer Woche nicht anders aussah und ich die Schnauze voll hatte. Weil mein Fotospot leicht erhöht liegt, vielleicht könnte ja ich über den Nebel hinwegfotografieren, aus dem optimalerweise nur die Kirchturmspitzen herausragen und es würde sogar richtig gut aussehen? Weil der Nebel sich bis zum Sonnenaufgang in zwei Stunden vielleicht eh wieder verzogen haben würde? Weil ich ja immerhin auch Sterne sehen konnte, wenn ich senkrecht nach oben geschaut habe? Wie sich herausstellen wird, waren meine Hoffnungen unbegründet, fast naiv. Als ich am Zielort ankomme, scheint sich das ganze noch verschlimmert zu haben, man sieht gar nichts.

  • IMG_3013
  • IMG_3022
 

Um dieses Ärgernis zumindest besser zu verstehen, es beim nächsten mal besser abschätzen und vielleicht ja sogar gestalterisch auch mal ausnutzen und vorhersagen zu können, folgt nun also die theoretische Auseinandersetzung:

 

Was ist Morgennebel?

Morgennebel ist nichts anderes, als eine Wolke in Bodenhöhe. Tausende winziger Wassertröpfchen schweben in der Luft und rauben so die Sicht.

 

Wann kommt Morgennebel?

Die kurze Antwort: besonders, wenn es am Tag zuvor warm war und eine sogenannte Hochdruckwetterlage besteht, also vor allem bei schwülem Wetter. Da gibt es meist keine oder nur wenige Wolken und wenn es dann Nacht wird, strahlt der Erdboden seine Wärme zurück ins Weltall. Dabei kühlen sich die bodennahen Luftschichten ab. Kalte Luft kann leider weniger Wasserdampf aufnehmen als warme Luft, d.h. ihr Taupunkt wird schneller erreicht, die Feuchtigkeit der Luft beträgt also 100% und der Wasserdampf kondensiert als flüssiges Wasser aus. Das sind dann die Tröpfchen, die den sichtbaren Nebel am nächsten Morgen bzw. schon in der Nacht bilden und mich die letzte Woche jedes mal den Sonnenaufgang gekostet haben.

 

Wann verschwindet er wieder?

Meine persönliche Antwort: leider nicht so schnell wie ich gerne hätte! Auch am heutigen Morgen konnte ich zwar erahnen, dass da hinterm Grau irgendwo die Sonne aufgeht, aber gesehen hab ich das nicht:

  • IMG_3032-2
  • IMG_3032
 

Wenn man sich mal bewusst macht, was es braucht um den Nebel wieder verschwinden zu lassen, wundert einen das aber auch nicht. Natürlich muss die kühle Luft wieder erwärmt werden, um mehr Wasserdampf aufnehmen zu können, so dass die Tröpfchen wieder verschwinden. Da der Boden seine Wärme über Nacht abgestrahlt hat, braucht es dafür die Sonne, und zwar viel davon! Der Nebel ist leider ein guter Reflektor und gibt etwa 90% der Sonnenstrahlung direkt wieder zurück. Die restlichen 10% müssen es also reißen und den Boden und die bodennahen Luftschichten wieder ausreichend stark erwärmen. Die logische Konsequenz ist also: bevor die Sonne nicht aufgeht, verschwindet auch der Nebel nicht! Und selbst dann braucht es erstmal noch etwas Zeit. 

Tja, dieses Wissen hätte mich heute ein paar Stunden länger schlafen lassen können. Wieder was gelernt!

P.S.: Es gibt allerdings noch einen Joker: den Wind. Wenn man Glück hat und dieser trockene Luft heranbläst, sinkt die durchschnittliche Luftfeuchtigkeit und der Nebel kann sich relativ rasch auflösen. Heute war es leider absolut windstill.

 

 

 

 


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    For other missions — it’s not so simple.

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    But those spacecraft also rely on their own kept time, Gramling said. Vehicles exploring deep into the solar system, for example, have to know — based on their own time scale — when they are approaching a planet in case the spacecraft needs to use that planetary body for navigational purposes, she added.

    For 50 years, scientists have also been able to observe atomic clocks that are tucked aboard GPS satellites, which orbit Earth about 12,550 miles (20,200 kilometers) away — or about one-nineteenth the distance between our planet and the moon.

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  • Kommentar-Link Brandonjex Dienstag, 15 April 2025 09:57 gepostet von Brandonjex

    Space, time: The continual question
    If time moves differently on the peaks of mountains than the shores of the ocean, you can imagine that things get even more bizarre the farther away from Earth you travel.
    Кракен тор
    To add more complication: Time also passes slower the faster a person or spacecraft is moving, according to Einstein’s theory of special relativity.

    Astronauts on the International Space Station, for example, are lucky, said Dr. Bijunath Patla, a theoretical physicist with the US National Institute of Standards and Technology, in a phone interview. Though the space station orbits about 200 miles (322 kilometers) above Earth’s surface, it also travels at high speeds — looping the planet 16 times per day — so the effects of relativity somewhat cancel each other out, Patla said. For that reason, astronauts on the orbiting laboratory can easily use Earth time to stay on schedule.
    https://kra30c.cc
    kra30 cc
    For other missions — it’s not so simple.

    Fortunately, scientists already have decades of experience contending with the complexities.

    Spacecraft, for example, are equipped with their own clocks called oscillators, Gramling said.

    “They maintain their own time,” Gramling said. “And most of our operations for spacecraft — even spacecraft that are all the way out at Pluto, or the Kuiper Belt, like New Horizons — (rely on) ground stations that are back on Earth. So everything they’re doing has to correlate with UTC.”
    But those spacecraft also rely on their own kept time, Gramling said. Vehicles exploring deep into the solar system, for example, have to know — based on their own time scale — when they are approaching a planet in case the spacecraft needs to use that planetary body for navigational purposes, she added.

    For 50 years, scientists have also been able to observe atomic clocks that are tucked aboard GPS satellites, which orbit Earth about 12,550 miles (20,200 kilometers) away — or about one-nineteenth the distance between our planet and the moon.

    Studying those clocks has given scientists a great starting point to begin extrapolating further as they set out to establish a new time scale for the moon, Patla said.

    “We can easily compare (GPS) clocks to clocks on the ground,” Patla said, adding that scientists have found a way to gently slow GPS clocks down, making them tick more in-line with Earth-bound clocks. “Obviously, it’s not as easy as it sounds, but it’s easier than making a mess.”

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