scholarly journals Effects of the North Atlantic Subtropical High on summertime precipitation organization in the southeast United States

2020 ◽  
Vol 40 (14) ◽  
pp. 5987-6001
Author(s):  
Rosana Nieto Ferreira ◽  
Thomas M. Rickenbach
Keyword(s):  
United States ◽  
North Atlantic ◽  
Subtropical High ◽  
Southeast United States ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

scholarly journals Influence of the North Atlantic Subtropical High on wet and dry sea-breeze events in North Carolina, United States

2017 ◽  
pp. 9 ◽  
Author(s):  
Nicholas T. Luchetti ◽  
Rosana Nieto Ferreira ◽  
Thomas M. Rickenbach ◽  
Mark R. Nissenbaum ◽  
Joel D. McAuliffe
Keyword(s):  
United States ◽  
North Carolina ◽  
North Atlantic ◽  
Convective Available Potential Energy ◽  
Sea Breeze ◽  
The United States ◽  
Subtropical High ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

The sea-breeze (SB) is an important source of summertime precipitation in North Carolina (NC, southeast United States). However, not all SB events produce precipitation. A climatology of wet and dry SB events in NC is used to investigate the conditions that are conducive to precipitation associated with the sea breeze. Radar imagery was used to detect 88 SB events that occurred along the NC coast between May-September of 2009-2012. The majority (85%) of SB events occurred during offshore flow (53%) or during flow that was parallel to the coast (22%). SB events were separated into dry (53%) and wet (47%) events and differences in the dynamic and thermodynamic parameters of the environment in which they formed were analyzed. Significant differences in dynamic and thermodynamic conditions were found. SB dry events occurred under stronger winds (6.00 ± 2.36 ms-1) than SB wet events (4.02 ± 2.16 ms-1). Moreover, during SB wet events larger values of convective available potential energy and lower values of convective inhibition were present, conditions that favor precipitation. Overall, the SB wet events accounted for 20-30% of the May-September precipitation along the NC coastal region. The position of the North Atlantic Subtropical High (NASH) controls both moisture availability and winds along the NC coast, thus providing a synoptic-scale control mechanism for SB precipitation. In particular, it was shown that when the NASH western ridge is located along the southeast coast of the United States, it causes a moist southwesterly flow along the NC coast that may favor the occurrence of SB wet events.

Impacts of the North Atlantic Subtropical High on Daily Summer Precipitation over the Conterminous United States

2021 ◽  
Author(s):  
Enrico Zorzetto ◽  
Laifang Li
Keyword(s):  
United States ◽  
North Atlantic ◽  
Daily Rainfall ◽  
Summer Precipitation ◽  
Subtropical High ◽  
Rainfall Events ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic ◽  
The Impact

AbstractBy modulating the moisture flux from ocean to adjacent land, the North Atlantic Subtropical High (NASH) western ridge significantly influences summer-season total precipitation over the Conterminous United States (CONUS). However, its influence on the frequency and intensity of daily rainfall events over the CONUS remains unclear. Here we introduce a Bayesian statistical model to investigate the impacts of the NASH western ridge position on key statistics of daily-scale summer precipitation, including the intensity of rainfall events, the probability of precipitation occurrence, and the probability of extreme values. These statistical quantities play a key role in characterizing both the impact of wet extremes (e.g., the probability of floods) and dry extremes. By applying this model to historical rain gauge records (1948-2019) covering the entire CONUS, we find that the western ridge of the NASH influences the frequency of rainfall as well as the distribution of rainfall intensities over extended areas of the CONUS. In particular, we find that the NASH ridge also modulates the frequency of extreme rainfall, especially that over part of the Southeast and upper Midwest. Our analysis underlines the importance of including the NASH western ridge position as a predictor for key statistical rainfall properties to be used for hydrological applications. This result is especially relevant for projecting future changes in daily rainfall regimes over the CONUS based on the predicted strengthening of the NASH in a warming climate.

Impacts of the North Atlantic subtropical high on interannual variation of summertime heat stress over the conterminous United States

2019 ◽  
Vol 53 (5-6) ◽  
pp. 3345-3359 ◽  
Author(s):  
Wenhong Li ◽  
Tian Zou ◽  
Laifang Li ◽  
Yi Deng ◽  
Victor T. Sun ◽  
...  
Keyword(s):  
United States ◽  
Heat Stress ◽  
North Atlantic ◽  
Interannual Variation ◽  
Subtropical High ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

scholarly journals Projection of Summer Precipitation over the Southeastern United States in the Superparameterized CCSM4

2015 ◽  
Vol 28 (20) ◽  
pp. 8052-8066 ◽  
Author(s):  
Xiaojie Zhu ◽  
Cristiana Stan
Keyword(s):  
United States ◽  
Soil Moisture ◽  
North Atlantic ◽  
Hydrological Cycle ◽  
Southeastern United States ◽  
Summer Precipitation ◽  
Subtropical High ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

Abstract Projections of the hydrological cycle over the southeastern United States are compared between CCSM4 and the superparameterized model (SP-CCSM4). Under the extreme forcing of the representative concentration pathway 8.5 (RCP8.5) climate change scenario, in Virginia, North Carolina, South Carolina, and Kentucky, SP-CCSM4 projects a decrease in summer precipitation, whereas the conventionally parameterized CCSM4 projects an increase in summer rainfall. The projected reduction in summer precipitation in SP-CCSM4 is due to the remote influence from the northwest intrusion of the North Atlantic subtropical high, as well as the local decrease of soil moisture content. Both models show that summer precipitation over the southern United States is characterized by a positive feedback with soil moisture. However, in CCSM4 rainfall increases with increasing soil moisture and in SP-CCSM4 rainfall decreases with decreasing soil moisture. The different representation of cloud processes in the two models yields different responses of precipitation to the latent heat flux changes over the southeastern United States. Moreover, multivariate EOF analyses in the two models suggest that the local land–atmosphere interactions have a stronger influence on the projected changes of precipitation over the southeastern United States than does the North Atlantic subtropical high.

scholarly journals Comments on “Changes to the North Atlantic Subtropical High and Its Role in the Intensification of Summer Rainfall Variability in the Southeastern United States”

2013 ◽  
Vol 26 (2) ◽  
pp. 679-682 ◽  
Author(s):  
Jeremy E. Diem
Keyword(s):  
United States ◽  
Global Warming ◽  
North Atlantic ◽  
Rainfall Variability ◽  
Southeastern United States ◽  
Summer Rainfall ◽  
Subtropical High ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

Abstract In a recent article, Li et al. examined changes in the summer-season location of the western ridge of the North Atlantic subtropical high from 1948 to 2007 because there has been an increase in interannual summer rainfall variability in the southeastern United States. The following major conclusions by Li et al. are incorrect: the western ridge has undergone a significant westward trend since the late 1970s; the western ridge had increased meridional movement during 1978–2007 compared to 1948–1977; and global warming appears to be contributing to the westward expansion of the western ridge. Results presented in this paper reveal that the western ridge has been moving eastward over the past three decades, there was no change in latitudinal variance, and a westward movement of the western ridge should not be linked to global warming.

scholarly journals Changes to the North Atlantic Subtropical High and Its Role in the Intensification of Summer Rainfall Variability in the Southeastern United States

2011 ◽  
Vol 24 (5) ◽  
pp. 1499-1506 ◽  
Author(s):  
Wenhong Li ◽  
Laifang Li ◽  
Rong Fu ◽  
Yi Deng ◽  
Hui Wang
Keyword(s):  
United States ◽  
North Atlantic ◽  
Rainfall Variability ◽  
Summer Precipitation ◽  
Summer Rainfall ◽  
Subtropical High ◽  
Intergovernmental Panel ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

Abstract This study investigates the changes of the North Atlantic subtropical high (NASH) and its impact on summer precipitation over the southeastern (SE) United States using the 850-hPa geopotential height field in the National Centers for Environmental Prediction (NCEP) reanalysis, the 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40), long-term rainfall data, and Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) model simulations during the past six decades (1948–2007). The results show that the NASH in the last 30 yr has become more intense, and its western ridge has displaced westward with an enhanced meridional movement compared to the previous 30 yr. When the NASH moved closer to the continental United States in the three most recent decades, the effect of the NASH on the interannual variation of SE U.S. precipitation is enhanced through the ridge’s north–south movement. The study’s attribution analysis suggested that the changes of the NASH are mainly due to anthropogenic warming. In the twenty-first century with an increase of the atmospheric CO2 concentration, the center of the NASH would be intensified and the western ridge of the NASH would shift farther westward. These changes would increase the likelihood of both strong anomalously wet and dry summers over the SE United States in the future, as suggested by the IPCC AR4 models.

scholarly journals Dynamical and thermodynamical coupling between the North Atlantic subtropical high and the marine boundary layer clouds in boreal summer

2017 ◽  
Vol 50 (7-8) ◽  
pp. 2457-2469 ◽  
Author(s):  
Wei Wei ◽  
Wenhong Li ◽  
Yi Deng ◽  
Song Yang ◽  
Jonathan H. Jiang ◽  
...  
Keyword(s):  
Boundary Layer ◽  
North Atlantic ◽  
Marine Boundary Layer ◽  
Subtropical High ◽  
Boreal Summer ◽  
Boundary Layer Clouds ◽  
North Atlantic Subtropical High ◽  
The North ◽  
The North Atlantic

Reply to “Comments on ‘Changes to the North Atlantic Subtropical High and Its Role in the Intensification of Summer Rainfall Variability in the Southeastern United States’”

2013 ◽  
Vol 26 (2) ◽  
pp. 683-688 ◽  
Author(s):  
Wenhong Li ◽  
Laifang Li ◽  
Rong Fu ◽  
Yi Deng ◽  
Hui Wang
Keyword(s):  
North Atlantic ◽  
Rainfall Variability ◽  
Southeastern United States ◽  
Summer Rainfall ◽  
Subtropical High ◽  
North Atlantic Subtropical High ◽  
The North ◽  
Westward Movement ◽  
The North Atlantic ◽  
Potential Impact

Abstract Recently Diem questioned the western ridge movement of the North Atlantic subtropical high (NASH) reported in a 2011 paper of Li et al. This reply shows more analysis that further strengthens the conclusions originally put forth by Li et al. Diem’’s analysis of the trend in the western ridge of the NASH was based on the data over a 30-yr period (1978–2007), whereas the main conclusions in Li et al. were drawn according to the data over a 60-yr period (1948–2007). Over the last 60 years, the NASH has shown a significant trend of westward movement, the meridional movement of the western ridge of the NASH has enhanced in the recent three decades, and the potential impact of global warming cannot be ruled out in an attempt to explain these changes of the NASH.

Sign in / Sign up

Export Citation Format

Share Document