Effect of First Order Chemical Reaction for Coriolis Force and Dust Particles for Small Reynolds Number in the Atmosphere Over Territory

α
Dr. Md. Abu Bkar Pk
Dr. Md. Abu Bkar Pk
σ
M. A. Bkar Pk
M. A. Bkar Pk
ρ
Ripan Roy
Ripan Roy
α University of Rajshahi University of Rajshahi

Send Message

To: Author

Effect of First Order Chemical Reaction for Coriolis Force and Dust Particles for Small Reynolds Number in the Atmosphere Over Territory

Article Fingerprint

ReserarchID

V41XS

Effect of First Order Chemical Reaction for Coriolis Force and Dust Particles for Small Reynolds Number in the Atmosphere Over Territory Banner

AI TAKEAWAY

Connecting with the Eternal Ground
  • English
  • Afrikaans
  • Albanian
  • Amharic
  • Arabic
  • Armenian
  • Azerbaijani
  • Basque
  • Belarusian
  • Bengali
  • Bosnian
  • Bulgarian
  • Catalan
  • Cebuano
  • Chichewa
  • Chinese (Simplified)
  • Chinese (Traditional)
  • Corsican
  • Croatian
  • Czech
  • Danish
  • Dutch
  • Esperanto
  • Estonian
  • Filipino
  • Finnish
  • French
  • Frisian
  • Galician
  • Georgian
  • German
  • Greek
  • Gujarati
  • Haitian Creole
  • Hausa
  • Hawaiian
  • Hebrew
  • Hindi
  • Hmong
  • Hungarian
  • Icelandic
  • Igbo
  • Indonesian
  • Irish
  • Italian
  • Japanese
  • Javanese
  • Kannada
  • Kazakh
  • Khmer
  • Korean
  • Kurdish (Kurmanji)
  • Kyrgyz
  • Lao
  • Latin
  • Latvian
  • Lithuanian
  • Luxembourgish
  • Macedonian
  • Malagasy
  • Malay
  • Malayalam
  • Maltese
  • Maori
  • Marathi
  • Mongolian
  • Myanmar (Burmese)
  • Nepali
  • Norwegian
  • Pashto
  • Persian
  • Polish
  • Portuguese
  • Punjabi
  • Romanian
  • Russian
  • Samoan
  • Scots Gaelic
  • Serbian
  • Sesotho
  • Shona
  • Sindhi
  • Sinhala
  • Slovak
  • Slovenian
  • Somali
  • Spanish
  • Sundanese
  • Swahili
  • Swedish
  • Tajik
  • Tamil
  • Telugu
  • Thai
  • Turkish
  • Ukrainian
  • Urdu
  • Uzbek
  • Vietnamese
  • Welsh
  • Xhosa
  • Yiddish
  • Yoruba
  • Zulu

Abstract

In the atmospheric boundary layer there are horizontal pressure gradient and Coriolis force to the velocity distribution signify that, the horizontal component of the velocity in the boundary layer turns left (right) with increasing height in the Southern (Northern) Hemisphere, downward (upward) motion occurs on the windward (lee) side of the mountain, and downward (upward) motion also occurs on the slope to the right (left) of the geostrophic wind in the Northern Hemisphere, whereas in the Southern Hemisphere upward (downward) motion occurs on the slope to the left (right) of the geostrophic wind. Using Navier-Stokes equations for threedimensional stationary flows, hydrostatic and continuity equations, the effects of first order reactant of Coriolis force and dust particles for small Reynolds number in the atmospheric boundary layer over territory is obtained.

References

15 Cites in Article
  1. M Lyberg,H Tryggeson (2007). An analytical solution of the Navier-Stokes equations for internal flows.
  2. D Chae,H Choe (1999). Regularity of solutions to the Navier-Stokes equations.
  3. Gunawan Nugroho,Ahmed Ali,Zainal Abdul Karim (2009). On a special class of analytical solutions to the three-dimensional incompressible Navier–Stokes equations.
  4. C Wang (1991). Exact solutions of the steady Navier-Stokes equations.
  5. K Thailert (2005). One Class of Regular Partially Invariant Solutions of the Navier–Stokes Equations.
  6. A Shapiro (1984). The use of an exact solution of the Navier-Stokes equations in a validation test of a.
  7. G Nugroho (2013). On analytical solutions to the threedimensional incompressible Navier-Stokes equations with general forcing functions and their relation to turbulence.
  8. M Bkar Pk,M Azad,M Sarker (2012). Decay of energy of MHD turbulence for four-point correlation.
  9. M Bkar Pk,M Azad,M Sarker (2013). Decay of dusty fluid MHD turbulence for four-point correlation in a rotating system.
  10. M Bkar Pk,M Sarker,M Azad (2013). Decay of MHD turbulence prior to the ultimate phase in presence of dust particle for four-point correlation.
  11. S Kao (1976). A Model for Turbulent Diffusion over Terrain.
  12. V Ekman (1905). On the influence of the earth's rotation on ocean currents.
  13. S Kao (1981). An analytical solution for three dimensional stationary flows in the atmospheric boundary layer over terrain.
  14. M Bkar Pk,Abdul Malek,M Azad (2015). 4-Point Correlations of Dusty Fluid MHD Turbulent Flow in a 1 st Order Chemical-Reaction.
  15. M Azad,Abdul Malek,M Bkar Pk (2015). 3-Point Distribution Functions in the Statistical Theory in MHD Turbulent Flow for Velocity, Magnetic Temperature and Concentration under going a First Order Reaction.

Funding

No external funding was declared for this work.

Conflict of Interest

The authors declare no conflict of interest.

Ethical Approval

No ethics committee approval was required for this article type.

Data Availability

Not applicable for this article.

How to Cite This Article

Dr. Md. Abu Bkar Pk. 2016. \u201cEffect of First Order Chemical Reaction for Coriolis Force and Dust Particles for Small Reynolds Number in the Atmosphere Over Territory\u201d. Global Journal of Science Frontier Research - H: Environment & Environmental geology GJSFR-H Volume 16 (GJSFR Volume 16 Issue H1): .

Download Citation

Issue Cover
GJSFR Volume 16 Issue H1
Pg. 39- 50
Journal Specifications

Crossref Journal DOI 10.17406/GJSFR

Print ISSN 0975-5896

e-ISSN 2249-4626

Keywords
Classification
GJSFR-H Classification: FOR Code: 059999p
Version of record

v1.2

Issue date

March 20, 2016

Language
en
Experiance in AR

Explore published articles in an immersive Augmented Reality environment. Our platform converts research papers into interactive 3D books, allowing readers to view and interact with content using AR and VR compatible devices.

Read in 3D

Your published article is automatically converted into a realistic 3D book. Flip through pages and read research papers in a more engaging and interactive format.

Article Matrices
Total Views: 3950
Total Downloads: 1963
2026 Trends
Related Research

Published Article

In the atmospheric boundary layer there are horizontal pressure gradient and Coriolis force to the velocity distribution signify that, the horizontal component of the velocity in the boundary layer turns left (right) with increasing height in the Southern (Northern) Hemisphere, downward (upward) motion occurs on the windward (lee) side of the mountain, and downward (upward) motion also occurs on the slope to the right (left) of the geostrophic wind in the Northern Hemisphere, whereas in the Southern Hemisphere upward (downward) motion occurs on the slope to the left (right) of the geostrophic wind. Using Navier-Stokes equations for threedimensional stationary flows, hydrostatic and continuity equations, the effects of first order reactant of Coriolis force and dust particles for small Reynolds number in the atmospheric boundary layer over territory is obtained.

Our website is actively being updated, and changes may occur frequently. Please clear your browser cache if needed. For feedback or error reporting, please email [email protected]

Request Access

Please fill out the form below to request access to this research paper. Your request will be reviewed by the editorial or author team.
X

Quote and Order Details

Contact Person

Invoice Address

Notes or Comments

This is the heading

Lorem ipsum dolor sit amet, consectetur adipiscing elit. Ut elit tellus, luctus nec ullamcorper mattis, pulvinar dapibus leo.

High-quality academic research articles on global topics and journals.

Effect of First Order Chemical Reaction for Coriolis Force and Dust Particles for Small Reynolds Number in the Atmosphere Over Territory

M. A. Bkar Pk
M. A. Bkar Pk
Ripan Roy
Ripan Roy

Research Journals