Transcript
![Page 1: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/1.jpg)
AULA 2
FUNDAMENTOS DE
TURBULÊNCIA ATMOSFÉRICA
![Page 2: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/2.jpg)
![Page 3: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/3.jpg)
![Page 4: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/4.jpg)
![Page 5: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/5.jpg)
![Page 6: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/6.jpg)
![Page 7: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/7.jpg)
![Page 8: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/8.jpg)
![Page 9: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/9.jpg)
![Page 10: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/10.jpg)
![Page 11: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/11.jpg)
![Page 12: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/12.jpg)
![Page 13: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/13.jpg)
![Page 14: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/14.jpg)
![Page 15: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/15.jpg)
![Page 16: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/16.jpg)
![Page 17: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/17.jpg)
![Page 18: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/18.jpg)
![Page 19: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/19.jpg)
![Page 20: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/20.jpg)
![Page 21: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/21.jpg)
![Page 22: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/22.jpg)
![Page 23: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/23.jpg)
![Page 24: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/24.jpg)
![Page 25: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/25.jpg)
![Page 26: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/26.jpg)
![Page 27: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/27.jpg)
![Page 28: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/28.jpg)
![Page 29: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/29.jpg)
![Page 30: MET 333 – AULA 3chuvaproject.cptec.inpe.br/portal/saoluis/curso/fisch/aula2.pdf · (2.13) An important simplification is possible in the atmospheric boundary layer where only the](https://reader033.vdocument.in/reader033/viewer/2022050610/5fb1e3d5f4983416d00c5c70/html5/thumbnails/30.jpg)
Conhecimento da Camada Limite Planetária baseado no tripé:
observações, ensaios em túnel de vento (tanque de água) e
modelagem atmosférica
AULA 2
FUNDAMENTOS DE
TURBULÊNCIA ATMOSFÉRICA
Conhecimento da Camada Limite Planetária baseado no tripé:
observações, ensaios em túnel de vento (tanque de água) e
modelagem atmosférica