Faịlụ:Annotated Skew T diagram.png
Otu nyochaa a ha:720 × 600 piksels Ndị ọzọ mkpebi:288 × 240 piksels | 576 × 480 piksels | 864 × 720 piksels.
Failụ si na nke mbu (864 × 720 pixel, ívù akwukwo orunótu: 97 KB, MIME nke: image/png)
Mmẹkụwátá
| Nkówá |
English: The altitude of clouds can be partially inferred by high relative humidity, where the dewpoint and temperature are close. The type of cloud is suggested by the stability of the atmosphere, determined by the steepness of the temperature profile compared to the adiabatic lapse rate. The underlying graph was downloaded from the University of Wyoming atmospheric soundings archive, http://weather.uwyo.edu/upperair/sounding.html. |
| Ǹgụ́ụ̀bọ̀chị̀ | |
| Mkpọlọ́gwụ̀ | Orü ọnwé |
| Odé ákwụ́kwọ́ | JeanBizHertzberg |
| Nke ya ozor | Derivative works of this file: Skew T annoté.png |
Nkwényé
I, the copyright holder of this work, hereby publish it under the following license:
This file is licensed under the Creative Commons Attribution-Share Alike 4.0 International license.
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Ịta nke usòrò
Bìri èhì/ogè k'ị hụ òtù ụ̀fa dị̀ m̀gbè ahụ̀.
| Èhì/Ogè | Mbọ-aka | Ógólógó na asaá | Òjìème | Nkwute | |
|---|---|---|---|---|---|
| dị ùgbu â | 23:47, 27 Ọktoba 2022 | | 864 × 720 (97 KB) | JeanBizHertzberg | Uploaded own work with UploadWizard |
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