The Experts below are selected from a list of 285 Experts worldwide ranked by ideXlab platform

Ibrahim Hoteit - One of the best experts on this subject based on the ideXlab platform.

  • Author Correction: Decadal trends in Red Sea Maximum Surface Temperature.
    Scientific reports, 2018
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper.

  • decadal trends in red sea Maximum Surface Temperature
    Scientific Reports, 2017
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    Ocean warming is a major consequence of climate change, with the Surface of the ocean having warmed by 0.11 °C decade−1 over the last 50 years and is estimated to continue to warm by an additional 0.6 – 2.0 °C before the end of the century1. However, there is considerable variability in the rates experienced by different ocean regions, so understanding regional trends is important to inform on possible stresses for marine organisms, particularly in warm seas where organisms may be already operating in the high end of their thermal tolerance. Although the Red Sea is one of the warmest ecosystems on earth, its historical warming trends and thermal evolution remain largely understudied. We characterized the Red Sea’s thermal regimes at the basin scale, with a focus on the spatial distribution and changes over time of sea Surface Temperature maxima, using remotely sensed sea Surface Temperature data from 1982 – 2015. The overall rate of warming for the Red Sea is 0.17 ± 0.07 °C decade−1, while the northern Red Sea is warming between 0.40 and 0.45 °C decade−1, all exceeding the global rate. Our findings show that the Red Sea is fast warming, which may in the future challenge its organisms and communities.

Veronica Chaidez - One of the best experts on this subject based on the ideXlab platform.

  • Author Correction: Decadal trends in Red Sea Maximum Surface Temperature.
    Scientific reports, 2018
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper.

  • decadal trends in red sea Maximum Surface Temperature
    Scientific Reports, 2017
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    Ocean warming is a major consequence of climate change, with the Surface of the ocean having warmed by 0.11 °C decade−1 over the last 50 years and is estimated to continue to warm by an additional 0.6 – 2.0 °C before the end of the century1. However, there is considerable variability in the rates experienced by different ocean regions, so understanding regional trends is important to inform on possible stresses for marine organisms, particularly in warm seas where organisms may be already operating in the high end of their thermal tolerance. Although the Red Sea is one of the warmest ecosystems on earth, its historical warming trends and thermal evolution remain largely understudied. We characterized the Red Sea’s thermal regimes at the basin scale, with a focus on the spatial distribution and changes over time of sea Surface Temperature maxima, using remotely sensed sea Surface Temperature data from 1982 – 2015. The overall rate of warming for the Red Sea is 0.17 ± 0.07 °C decade−1, while the northern Red Sea is warming between 0.40 and 0.45 °C decade−1, all exceeding the global rate. Our findings show that the Red Sea is fast warming, which may in the future challenge its organisms and communities.

Francis E. Kennedy - One of the best experts on this subject based on the ideXlab platform.

  • Temperature Rise at the Sliding Contact Interface for a Coated Semi-Infinite Body
    Journal of Tribology, 1993
    Co-Authors: Xuefeng Tian, Francis E. Kennedy
    Abstract:

    In this paper, a three-dimensional model of a semi-infinite layered body is used to predict steady-state Maximum Surface Temperature rise at the sliding contact interface for the entire range of Peclet number. A set of semi-empirical solutions for Maximum Surface Temperature problems of sliding layered bodies is obtained by using integral transform, finite element, heuristic and multivariable regression techniques. Two dimensionless parameters, A and Dp, which relate to coating thickness, contact size, sliding speed and thermal properties of both coating and substrate materials, are found to be the critical factors determining the effect of Surface film on the Surface Temperature rise at a sliding contact interface

Denis Dreano - One of the best experts on this subject based on the ideXlab platform.

  • Author Correction: Decadal trends in Red Sea Maximum Surface Temperature.
    Scientific reports, 2018
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper.

  • decadal trends in red sea Maximum Surface Temperature
    Scientific Reports, 2017
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    Ocean warming is a major consequence of climate change, with the Surface of the ocean having warmed by 0.11 °C decade−1 over the last 50 years and is estimated to continue to warm by an additional 0.6 – 2.0 °C before the end of the century1. However, there is considerable variability in the rates experienced by different ocean regions, so understanding regional trends is important to inform on possible stresses for marine organisms, particularly in warm seas where organisms may be already operating in the high end of their thermal tolerance. Although the Red Sea is one of the warmest ecosystems on earth, its historical warming trends and thermal evolution remain largely understudied. We characterized the Red Sea’s thermal regimes at the basin scale, with a focus on the spatial distribution and changes over time of sea Surface Temperature maxima, using remotely sensed sea Surface Temperature data from 1982 – 2015. The overall rate of warming for the Red Sea is 0.17 ± 0.07 °C decade−1, while the northern Red Sea is warming between 0.40 and 0.45 °C decade−1, all exceeding the global rate. Our findings show that the Red Sea is fast warming, which may in the future challenge its organisms and communities.

Susana Agusti - One of the best experts on this subject based on the ideXlab platform.

  • Author Correction: Decadal trends in Red Sea Maximum Surface Temperature.
    Scientific reports, 2018
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper.

  • decadal trends in red sea Maximum Surface Temperature
    Scientific Reports, 2017
    Co-Authors: Veronica Chaidez, Denis Dreano, Susana Agusti, Carlos M Duarte, Ibrahim Hoteit
    Abstract:

    Ocean warming is a major consequence of climate change, with the Surface of the ocean having warmed by 0.11 °C decade−1 over the last 50 years and is estimated to continue to warm by an additional 0.6 – 2.0 °C before the end of the century1. However, there is considerable variability in the rates experienced by different ocean regions, so understanding regional trends is important to inform on possible stresses for marine organisms, particularly in warm seas where organisms may be already operating in the high end of their thermal tolerance. Although the Red Sea is one of the warmest ecosystems on earth, its historical warming trends and thermal evolution remain largely understudied. We characterized the Red Sea’s thermal regimes at the basin scale, with a focus on the spatial distribution and changes over time of sea Surface Temperature maxima, using remotely sensed sea Surface Temperature data from 1982 – 2015. The overall rate of warming for the Red Sea is 0.17 ± 0.07 °C decade−1, while the northern Red Sea is warming between 0.40 and 0.45 °C decade−1, all exceeding the global rate. Our findings show that the Red Sea is fast warming, which may in the future challenge its organisms and communities.