Title
Solar Dynamic Effects on Stratospheric Ozone Variations in the Tropics: Contributions of zonal winds, length of day, atmospheric,Used
Sold by Ergodebooks, an authorized reseller.
Returns accepted within 30 days | support@ergodebooks.com
Shipping Information
- Free Standard Shipping — United States only
- Processing Time: 1–3 business days
- Estimated Delivery: 3–5 business days after dispatch
- Double-boxed, fully insured & discreetly packaged
- Tracking number sent via email once dispatched
- Orders over $250 require signature upon delivery. Taxes calculated at checkout.
Returns & Refund
Returns accepted within 30 days of delivery.
Damaged or Defective Item
Free return shipping + replacement or full refund
Wrong Item Received
Free return shipping + replacement or full refund
Change of Mind
Return shipping at customer's expense · 25% restocking fee applies
Ozone variations have been a serious problem facing most scientists as its depletion continues to constitute menace to the world. Nigeria is in the tropical region where little or no research work involving solar dynamical processes effects on ozone changes has been carried out probably due to the earlier assertion that zonal winds were weak in the tropics. This work establishes that the changes in Atmospheric Angular Momentum (AAM) caused by the changes in the Length of Day (LOD) transfers ozone (O3) by means of zonal wind from the upper troposphere to the lower stratosphere in the tropics. And since O3 transportation is distinctly enhanced by the zonal winds in Nigeria, the zonal winds are not weak in the tropics. However, this work affirms that O3 variations are more pronounced in the higher than in the low latitude
⚠️ WARNING (California Proposition 65):
This product may contain chemicals known to the State of California to cause cancer, birth defects, or other reproductive harm.
For more information, please visit www.P65Warnings.ca.gov.