课题基金 / 基金详情

New Tools for Quantifying Cloud Response to Varying Climate States

New Tools for Quantifying Cloud Response to Varying Climate States
用于量化云对不同气候状态的响应的新工具
批准号:
2022941
负责人:
Timothy Garrett
金额:
$55.61万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2020
资助国家:
美国
项目状态:
已结题
起止时间:
2020-11-01 至 2024-10-31

项目摘要

项目成果

Timothy Garrett的其他基金

相似基金

相关文献

中文摘要
翻译
点击翻译按钮获取中文摘要
英文摘要
Clouds play a central role in Earth's climate as they regulate both the amount of sunlight reaching the Earth and the amount of infrared radation the Earth emits to space. But the climatic effect of clouds is an aggregate effect over a bewildering variety of cloud types, structures, and sizes. In principle this aggregate effect can be calculated on a cloud-by-cloud basis, simulating all clouds in detail and then adding up their individual contributions. But such simulations are impractical and in any case do not provide a satisfactory explanation for cloud behaviors. An alternative approach is to look for ways in which the fine-scale properties of clouds are determined, at least approximately, by the bulk properties of the large-scale atmosphere. This approach has the advantage of focusing on cloud properties which are likely to be influenced by climate change and may act to amplify or moderate the amount of warming caused by greenhouse gas increases.In recent work the PIs have developed a theory in which the stratification of the large-scale atmosphere exerts a thermodynamic constraint on the fine-scale complexity of tropical convective clouds. The theory assumes a quasi-equilibrium state in which convective potential energy generated by solar heating at ground level is dissipated by horizontal turbulent mixing between rising air in clouds and surrounding clear air, which has lower potential energy. Since the sides of a cloud constitute a boundary through which mixing occurs across a potential energy drop, the theory implies a relationship between the length of cloud perimeter on a surface of atmospheric potential energy (specifically saturated static energy) and the stability of the atmosphere to overturning motions at that level. In quasi-equilibrium this relationship further implies that the number of clouds with a given perimeter length is inversely proportional to that perimeter length. Also, the mass flux through the sides of a cloud is related to the potential energy difference between the cloud and its environment. This relationship can be used to show that clouds of high convective potential energy are exponentially more rare than clouds of lower potential energy (a form of the Boltzmann distribution).Work under this award tests the theory's predictions regarding the perimeter and energy dependence of cloud occurrence using satellite observations and model simulations. Further work addresses the extent to which the relationship between cloud number and perimeter length can be used to infer the number of clouds with a given horizontal area (possibly following Korcak's law), as cloud area has a direct connection to the climatic effects of clouds. Finally, the implications of the theory for changes in tropical convective clouds in response to climate change will be explored. Atmospheric stability is expected to increase in a warmer climate, and the relationship between stability and perimeter length suggests that warming will increase cloud number and total perimeter. But some work is required to reconcile this result with other thermodynamically-based arguments for changes in tropical cloud cover with warming.The work has societal relevance given concerns regarding the severity of climate change and its impacts on people and the environment. Clouds are perhaps the greatest source of uncertainty in efforts to determine the amount of warming produced by increases in greenhouse gas concentrations, and the relationships between fine-scale cloud properties and large-scale atmospheric conditions examined here could help to reduce this uncertainty. The project includes participants at the University of Lille and thus promotes international research collaboration. It also provides support and training to two graduate students and one undergraduate, thereby building the future workforce in this research area.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
期刊论文(1)
专著(0)
科研奖励(0)
会议论文
DOI: 10.5194/acp-24-109-2024
发表时间: 2024
期刊: Atmospheric Chemistry and Physics
影响因子: 6.3
作者: [DeWitt, Thomas D., Garrett, Timothy J., Rees, Karlie N., Bois, Corey, Krueger, Steven K., Ferlay, Nicolas]
通讯作者: Ferlay, Nicolas
Observational Evaluation of the Effects of Atmospheric Temperature and Turbulence on Hydrometeor Fallspeed
  • 批准号:
    2210179
  • 项目类别:
    Standard Grant
  • 资助金额:
    $74.7万
  • 财政年份:
    2022
  • 负责人:
    Timothy Garrett
  • 依托单位:
Observational and Theoretical Investigations Related to Hydrometeor Settling in Turbulent Air
  • 批准号:
    1841870
  • 项目类别:
    Standard Grant
  • 资助金额:
    $49.9万
  • 财政年份:
    2019
  • 负责人:
    Timothy Garrett
  • 依托单位:
Impacts of distant pollution sources on microphysical transitions in Arctic clouds
  • 批准号:
    1303965
  • 项目类别:
    Standard Grant
  • 资助金额:
    $45.08万
  • 财政年份:
    2013
  • 负责人:
    Timothy Garrett
  • 依托单位:
Collaborative Research: The Wasatch Hydrometeor Aggregation and Riming Experiment
  • 批准号:
    1127692
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $44.81万
  • 财政年份:
    2011
  • 负责人:
    Timothy Garrett
  • 依托单位:
海外基金