Impacts of anthropogenic forcing and internal variability at the watershed scale - going from the daily to the hourly time scale

流域尺度上的人为强迫和内部变异的影响 - 从每日到每小时的时间尺度

• 批准号: RGPIN-2020-07242
• 负责人: Brissette, Francois
• 金额: $ 3.13万
• 依托单位: École de technologie supérieure
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2021
• 资助国家: 加拿大
• 起止时间: 2021-01-01 至 2022-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=741041
• 关键词: Impacts; anthropogenic; forcing; internal; variability

Climate change resulting from the anthropogenic impact on radiative forcing is now well established. In addition to increases in projected surface temperatures, the changes will affect all major components of the water cycle, including variability and intensity of rainfall at various spatial and temporal scales. The knowledge of the impacts of these changes comes largely from general circulation and earth system models. However, due to the limitations related to the available computing power, the outputs of these models have mostly been available at the daily time-step until recently. Changes at the sub-daily scales are therefore less well documented. Nevertheless, releases of higher-resolution regional climate models (convection-permitting or not) indicate that the impacts of anthropogenic forcing will be greater for short-duration and intense rainfall. We can thus predict a disproportionate impact on small watersheds whose hydrological response is rapid and commensurable with that of convective precipitation systems. Similarly, we can also predict a decrease in the impact of snowmelt related floods to those related to summer fall precipitation over small watersheds (<1000 km2). In hydrology, these results point to major impacts towards small rural and urbanized watersheds. The potential impacts of anthropogenic forcing change on the hydrology of these basins have been poorly studied for two main reasons: 1-There is no reliable hydrometeorological database at sub-daily time steps in North America (as well as in the majority of the world, except for a few European countries) to study these watersheds in sufficient numbers; 2-There are still few climate models whose main outputs (e.g. temperature and precipitation) are available at the sub-daily time steps. This research program specifically aims to fill this knowledge gap by using the tools and methodologies developed within our research laboratory and elsewhere to study the impacts of climate change at the daily time step on small to medium-size watersheds. These tools and methods will be combined with the use of new databases and outputs of climate models with high temporal and spatial resolution to thus be able to tackle the study of small to mdieum-size watersheds up to the hourly time step and below.

人类活动对辐射强迫的影响所导致的气候变化现已得到充分证实。除了预计地表温度上升之外，这些变化还将影响水循环的所有主要组成部分，包括不同时空尺度的降雨变化和强度。关于这些变化影响的知识主要来自大气环流和地球系统模型。然而，由于与可用计算能力相关的限制，直到最近这些模型的输出大多以每日时间步长提供。因此，次日尺度的变化记录较少。然而，更高分辨率的区域气候模型（是否允许对流）的发布表明，人为强迫对短时强降雨的影响将更大。因此，我们可以预测对小流域的影响不成比例，这些流域的水文响应迅速且与对流降水系统的响应相当。同样，我们还可以预测小流域（<1000 km2）上与融雪相关的洪水的影响将减少与夏季秋季降水相关的影响。在水文学方面，这些结果表明对小型农村和城市化流域的重大影响。由于两个主要原因，人为强迫变化对这些流域水文的潜在影响研究很少： 1-北美（以及世界大部分地区）没有可靠的次日时间步长水文气象数据库。除少数欧洲国家外）对这些流域进行足够数量的研究； 2-仍然有少数气候模型的主要输出（例如温度和降水）可在亚日时间步长获得。该研究计划的具体目的是通过使用我们的研究实验室和其他地方开发的工具和方法来填补这一知识空白，以研究气候变化在每日时间步长对中小型流域的影响。这些工具和方法将与新数据库的使用以及具有高时间和空间分辨率的气候模型输出相结合，从而能够解决每小时时间步长及以下的中小型流域的研究。