Regional Structure

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Brian J Soden - One of the best experts on this subject based on the ideXlab platform.

  • effect of remote sea surface temperature change on tropical cyclone potential intensity
    Nature, 2007
    Co-Authors: Gabriel A Vecchi, Brian J Soden
    Abstract:

    The response of tropical cyclone activity to global warming is poorly understood. It is often assumed that warmer sea surface temperatures favour cyclone development and intensification, but this may not be the case as so many other factors are involved. Gabriel Vecchi and Brian Soden explore the relationship between changes in sea-surface temperature and a measure called 'tropical cyclone potential intensity', which provides an upper limit on cyclone intensity. They find that changes in potential intensity are closely related to the Regional Structure of warming, rather than local sea surface temperature — regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. This suggests that the response of tropical cyclone activity to natural climate variations, which tend to involve localized changes in sea surface temperature, may be larger (per unit local sea surface temperature change) than the response to the more uniform patterns of warming induced by greenhouse gases. The relationship between changes in sea surface temperature and a measure called 'tropical cyclone potential intensity', which provides an upper bound on cyclone intensity, is explored. It is found that changes in potential intensity are closely related to the Regional Structure of warming, rather than local sea surface temperature — regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. The response of tropical cyclone activity to global warming is widely debated1,2,3,4,5,6,7,8,9,10. It is often assumed that warmer sea surface temperatures provide a more favourable environment for the development and intensification of tropical cyclones, but cyclone genesis and intensity are also affected by the vertical thermodynamic properties of the atmosphere1,10,11,12,13. Here we use climate models and observational reconstructions to explore the relationship between changes in sea surface temperature and tropical cyclone ‘potential intensity’—a measure that provides an upper bound on cyclone intensity10,11,12,13,14 and can also reflect the likelihood of cyclone development15,16. We find that changes in local sea surface temperature are inadequate for characterizing even the sign of changes in potential intensity, but that long-term changes in potential intensity are closely related to the Regional Structure of warming; regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. We use this relationship to reconstruct changes in potential intensity over the twentieth century from observational reconstructions of sea surface temperature. We find that, even though tropical Atlantic sea surface temperatures are currently at a historical high, Atlantic potential intensity probably peaked in the 1930s and 1950s, and recent values are near the historical average. Our results indicate that—per unit local sea surface temperature change—the response of tropical cyclone activity to natural climate variations, which tend to involve localized changes in sea surface temperature, may be larger than the response to the more uniform patterns of greenhouse-gas-induced warming.

  • effect of remote sea surface temperature change on tropical cyclone potential intensity
    Nature, 2007
    Co-Authors: Gabriel A Vecchi, Brian J Soden
    Abstract:

    The response of tropical cyclone activity to global warming is widely debated. It is often assumed that warmer sea surface temperatures provide a more favourable environment for the development and intensification of tropical cyclones, but cyclone genesis and intensity are also affected by the vertical thermodynamic properties of the atmosphere. Here we use climate models and observational reconstructions to explore the relationship between changes in sea surface temperature and tropical cyclone 'potential intensity'--a measure that provides an upper bound on cyclone intensity and can also reflect the likelihood of cyclone development. We find that changes in local sea surface temperature are inadequate for characterizing even the sign of changes in potential intensity, but that long-term changes in potential intensity are closely related to the Regional Structure of warming; regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. We use this relationship to reconstruct changes in potential intensity over the twentieth century from observational reconstructions of sea surface temperature. We find that, even though tropical Atlantic sea surface temperatures are currently at a historical high, Atlantic potential intensity probably peaked in the 1930s and 1950s, and recent values are near the historical average. Our results indicate that--per unit local sea surface temperature change--the response of tropical cyclone activity to natural climate variations, which tend to involve localized changes in sea surface temperature, may be larger than the response to the more uniform patterns of greenhouse-gas-induced warming.

Gabriel A Vecchi - One of the best experts on this subject based on the ideXlab platform.

  • effect of remote sea surface temperature change on tropical cyclone potential intensity
    Nature, 2007
    Co-Authors: Gabriel A Vecchi, Brian J Soden
    Abstract:

    The response of tropical cyclone activity to global warming is poorly understood. It is often assumed that warmer sea surface temperatures favour cyclone development and intensification, but this may not be the case as so many other factors are involved. Gabriel Vecchi and Brian Soden explore the relationship between changes in sea-surface temperature and a measure called 'tropical cyclone potential intensity', which provides an upper limit on cyclone intensity. They find that changes in potential intensity are closely related to the Regional Structure of warming, rather than local sea surface temperature — regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. This suggests that the response of tropical cyclone activity to natural climate variations, which tend to involve localized changes in sea surface temperature, may be larger (per unit local sea surface temperature change) than the response to the more uniform patterns of warming induced by greenhouse gases. The relationship between changes in sea surface temperature and a measure called 'tropical cyclone potential intensity', which provides an upper bound on cyclone intensity, is explored. It is found that changes in potential intensity are closely related to the Regional Structure of warming, rather than local sea surface temperature — regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. The response of tropical cyclone activity to global warming is widely debated1,2,3,4,5,6,7,8,9,10. It is often assumed that warmer sea surface temperatures provide a more favourable environment for the development and intensification of tropical cyclones, but cyclone genesis and intensity are also affected by the vertical thermodynamic properties of the atmosphere1,10,11,12,13. Here we use climate models and observational reconstructions to explore the relationship between changes in sea surface temperature and tropical cyclone ‘potential intensity’—a measure that provides an upper bound on cyclone intensity10,11,12,13,14 and can also reflect the likelihood of cyclone development15,16. We find that changes in local sea surface temperature are inadequate for characterizing even the sign of changes in potential intensity, but that long-term changes in potential intensity are closely related to the Regional Structure of warming; regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. We use this relationship to reconstruct changes in potential intensity over the twentieth century from observational reconstructions of sea surface temperature. We find that, even though tropical Atlantic sea surface temperatures are currently at a historical high, Atlantic potential intensity probably peaked in the 1930s and 1950s, and recent values are near the historical average. Our results indicate that—per unit local sea surface temperature change—the response of tropical cyclone activity to natural climate variations, which tend to involve localized changes in sea surface temperature, may be larger than the response to the more uniform patterns of greenhouse-gas-induced warming.

  • effect of remote sea surface temperature change on tropical cyclone potential intensity
    Nature, 2007
    Co-Authors: Gabriel A Vecchi, Brian J Soden
    Abstract:

    The response of tropical cyclone activity to global warming is widely debated. It is often assumed that warmer sea surface temperatures provide a more favourable environment for the development and intensification of tropical cyclones, but cyclone genesis and intensity are also affected by the vertical thermodynamic properties of the atmosphere. Here we use climate models and observational reconstructions to explore the relationship between changes in sea surface temperature and tropical cyclone 'potential intensity'--a measure that provides an upper bound on cyclone intensity and can also reflect the likelihood of cyclone development. We find that changes in local sea surface temperature are inadequate for characterizing even the sign of changes in potential intensity, but that long-term changes in potential intensity are closely related to the Regional Structure of warming; regions that warm more than the tropical average are characterized by increased potential intensity, and vice versa. We use this relationship to reconstruct changes in potential intensity over the twentieth century from observational reconstructions of sea surface temperature. We find that, even though tropical Atlantic sea surface temperatures are currently at a historical high, Atlantic potential intensity probably peaked in the 1930s and 1950s, and recent values are near the historical average. Our results indicate that--per unit local sea surface temperature change--the response of tropical cyclone activity to natural climate variations, which tend to involve localized changes in sea surface temperature, may be larger than the response to the more uniform patterns of greenhouse-gas-induced warming.

Aleš Snoj - One of the best experts on this subject based on the ideXlab platform.

  • Regional Structure despite limited mtDNA sequence diversity found in the endangered Huchen, Hucho hucho (Linnaeus, 1758)
    Hydrobiologia, 2010
    Co-Authors: Steven Weiss, Saša Marić, Aleš Snoj
    Abstract:

    We evaluate the hypothesis of no geographic Structure in the Huchen (Hucho hucho), a large, predatory salmonid endemic to the Danube basin. Forty-seven individuals sampled from throughout the Huchen’s native range were genetically characterized. Extremely limited sequence diversity across 1,800 bases of mtDNA (the complete control region and partial NADH-1 subunit) evidenced by four closely related mtDNA haplotypes was found. Nonetheless, the geographic distribution of mtDNA repeats (5–10, 82-bp long copies per individual) as well as allelic diversity across two microsatellite loci indicated large-scale geographic Structure between the north-western (Austria and Slovenia) distribution area and eastern (Slovakia and Ukraine) or southern (Bosnia-Herzegovina and Montenegro) sample sites. An extremely slow rate of substitution for the H. hucho mtDNA is considered along with the alternative hypotheses to explain the limited mtDNA diversity. Considering the Regional genetic Structure implied by our data, we advocate restrictions on the transport of brood fish or yearlings across the range of the species distribution and sale of Huchen across international boundaries. Future genetic analysis to support local conservation and monitoring efforts must focus on developing a high-resolution screen that may be applied to identify hatchery versus naturally reproduced individuals in the wild.

Martin Jacob - One of the best experts on this subject based on the ideXlab platform.

  • corporate tax enforcement externalities and the banking sector
    Journal of Accounting Research, 2020
    Co-Authors: John Gallemore, Martin Jacob
    Abstract:

    We explore whether corporate tax enforcement can affect bank lending. Specifically, we hypothesize that tax enforcement efforts aimed at small and midsized enterprises (SME) can improve their information environments, which in turn could lead to increased bank commercial lending. Exploiting the Regional Structure employed by the IRS until 1999, we find that the corporate tax return audit probability for SMEs is associated with greater commercial lending growth for Regionally focused banks. We find similar evidence when exploiting the IRS reorganization from a Regional to federal system in 2000. Further results show that tax enforcement's impact on SME informational environments is at least partially responsible for this association: The impact of tax auditing on bank lending is stronger for banks facing greater informational disadvantages and in areas where SMEs face greater hold‐up problems. Finally, we find that the tax audit rate is positively associated with loan portfolio quality, suggesting that tax enforcement can lead to better loan decisions. Our findings are consistent with the tax authority's mandate having important externalities on bank lending and SME access to capital, suggesting that the benefits to tax enforcement go beyond improving tax collection.

  • corporate tax enforcement externalities and the banking sector
    Social Science Research Network, 2020
    Co-Authors: John Gallemore, Martin Jacob
    Abstract:

    We explore whether corporate tax enforcement can affect bank lending. Specifically, we hypothesize that tax enforcement efforts aimed at small and midsized enterprises (SME) can improve their information environments, which in turn could lead to increased bank commercial lending. Exploiting the Regional Structure employed by the IRS until 1999, we find that the corporate tax return audit probability for SMEs is associated with greater commercial lending growth for Regionally focused banks. We find similar evidence when exploiting the IRS reorganization from a Regional to federal system in 2000 as an exogenous change to tax enforcement at the district level. Further results show that tax enforcement’s impact on SME informational environments is at least partially responsible for this association: the impact of tax auditing on bank lending is stronger for banks facing greater informational disadvantages and in areas where SMEs face greater hold-up problems. Finally, we find that the tax audit rate is positively associated with loan portfolio quality, suggesting that tax enforcement can lead to better loan decisions. Our findings are consistent with the tax authority’s mandate having important externalities on bank lending and SME access to capital, suggesting that the benefits to tax enforcement go beyond improving tax collection.

Steven Weiss - One of the best experts on this subject based on the ideXlab platform.

  • Regional Structure despite limited mtDNA sequence diversity found in the endangered Huchen, Hucho hucho (Linnaeus, 1758)
    Hydrobiologia, 2010
    Co-Authors: Steven Weiss, Saša Marić, Aleš Snoj
    Abstract:

    We evaluate the hypothesis of no geographic Structure in the Huchen (Hucho hucho), a large, predatory salmonid endemic to the Danube basin. Forty-seven individuals sampled from throughout the Huchen’s native range were genetically characterized. Extremely limited sequence diversity across 1,800 bases of mtDNA (the complete control region and partial NADH-1 subunit) evidenced by four closely related mtDNA haplotypes was found. Nonetheless, the geographic distribution of mtDNA repeats (5–10, 82-bp long copies per individual) as well as allelic diversity across two microsatellite loci indicated large-scale geographic Structure between the north-western (Austria and Slovenia) distribution area and eastern (Slovakia and Ukraine) or southern (Bosnia-Herzegovina and Montenegro) sample sites. An extremely slow rate of substitution for the H. hucho mtDNA is considered along with the alternative hypotheses to explain the limited mtDNA diversity. Considering the Regional genetic Structure implied by our data, we advocate restrictions on the transport of brood fish or yearlings across the range of the species distribution and sale of Huchen across international boundaries. Future genetic analysis to support local conservation and monitoring efforts must focus on developing a high-resolution screen that may be applied to identify hatchery versus naturally reproduced individuals in the wild.