Ocean circulation is a pivotal component of Earth's climate system, facilitating the transfer of heat from the equator to the poles and influencing global weather patterns. Driven by wind patterns, temperature gradients, and the Coriolis effect due to Earth's rotation, surface currents are primarily wind-driven, while deeper currents are shaped by variations in water density (thermohaline circulation). These currents play a critical role in distributing nutrients and heat throughout the oceans, profoundly impacting marine ecosystems and climate stability worldwide. Understanding ocean circulation dynamics is essential for predicting climate change impacts, sea-level rise, and ensuring sustainable management of marine resources. Ongoing research continuously enhances our comprehension of these intricate processes, pivotal for environmental conservation and informed policy-making.
Title : Geotechnical ground investigation
Myint Win Bo, Toronto Metropolitan University , Canada
Title : Simultaneous Global Climate Change "Heat Waves" and microwave and radio-wave from Solar Flares
Shozo Yanagida, Osaka University, Japan
Title : How subsurface waters record the earth’s history
Leonid Anisimov, Volgograd State University, Russian Federation
Title : Landslides.Rainfall one of the main triggering factors in the mountainous regions of Puebla, Mexico.
Oscar Andres Cuanalo Campos, Universidad Popular Autónoma del Estado de Puebla, Mexico
Title : Geo Education exploratory learning sessions on field and underwater
Martina Gaglioti, LIPU, Italy
Title : Linking between color and element concentration for Fluorite: An optical spectroscopic approach
Ali Almohammed, Pandit Deendayal Energy University, India