International Business Machines Corporation

Michael F Baryla

Aaron K Baughman

Mauro Marzorati

Ahmed M Nassar

During a live stream of a main content to a user, a biometric response of the user is measured during a first streamed portion of the main content. The biometric response is analyzed to detect an event in the first streamed portion of the main content. The biometric response of the user during the event indicates that the event is a user-specific climactic event. Based on the analysis, a user-specific set of feature values is computed that are representative of the user-specific climactic event in the first streamed portion of the main content. A user-specific non-climactic period is forecasted in a future portion of the live stream during which a likelihood of an occurrence of any user-specific climactic event is below a threshold likelihood. A secondary content is inserted during the user-specific non-climactic period.

Individualized dynamic insertion of secondary content in live streaming

From a live streaming of a main content, an already streamed portion of the main content is analyzed to identify an occurrence of a climactic event in the main content. Based on the analysis, a set is constructed of feature values that are representative of the climactic event in the already streamed portion of the main content. A non-climactic period is forecasted during which a likelihood of an occurrence of any climactic event is below a threshold likelihood. A secondary content is inserted in the live streaming of the main content during the non-climactic period, such that a likelihood of the secondary content insertion interrupting the live streaming during a second climactic event is less than a second threshold of likelihood. The live streaming of the main content is continued after the secondary content is completely transmitted in the live streaming.

Intelligent insertion of secondary content in live streaming

A non-climactic period is forecasted during a live streaming of a main content, where a likelihood of an occurrence of any climactic event in the non-climactic period is below a threshold likelihood, and where a second content is inserted during the non-climactic period. A validation is requested from a first user of the live streaming, of the forecasted non-climactic period and a first response to the request is received from the first user. Based on the first response, a first rank of the first user is computed relative to another user in a group of responding users. A first dynamic delay period that has an inverse relationship with the first rank is computed for the first user. A first transmission of a future portion of the live streaming to the first user is delayed by at least the first dynamic delay period.

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Cary, NC, United States of America

Michael F Baryla