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Zusammenfassung Jetstream, Wasser in der Atmosphäre

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Jetstream; Wasser in der Atmosphäre, Aggregatzustände

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Written for

Institution
Secondary school
Study
Gymnasium
Course
School year
1

Document information

Uploaded on
January 25, 2022
Number of pages
1
Written in
2021/2022
Type
Summary

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Content preview

Der Jetstream lstranistroml



-
starker Hohenwird 1400km/hI

-
im Obersten Teil der troposphere letw .
12km Hotel

-
Westwindband

-
went von West nach Ost

>
umspannt Erde




starker Pctarwirbel schwoerer Polarwirbel




§É§ p¥☒xn
""" "" "^ """ " """"




>




Wasser in der Atmosphere


BB wcirmewirofreigesetzt
wasserdampf MM weirmewirdaufgenommen
( gasFormiga onsichtbar )

> on

Verdun
stung sublimation
ctonoensation Deposition
<
°

Wasser Schmelzer
F-is
<
( floss" 91 2- B. Wolken
. troopfchen ( fest -




, z . B. E-isKristake ca .
/ too mm 0
>
Moo mm 0 in Wasser Wolken)
Gefrieren in Eiswolkenl




-
Weasel der Aggregatzostande
>
Energie wird freigesetzto.geburden


>
grope warm emerges Konner in der Atmosphere gespeicne.tt/transportiert1freigesetz-t werden




absolute Feucnte : in einem bestimmtenluftoowmenuorhanoeneoasseroampfmeng.ee / Was ist da ? /
- .




ing / MY
-
maximale Feucht e : .
maximal aufzonehmender Oasserdampf (was cionnte da Sein ? )
( abh .
µ . Temperaturf



-

relative Luftfeucntigkeit : -
Uernciltnis absolutes & Max .
Feucht e ( in 44 ( vernalthis)




rel .
=ff¥ .
100
$3.62
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