Erik T. Swenson

ORCID: 0000-0003-2901-5540
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About
Contact & Profiles
Research Areas
  • Climate variability and models
  • Tropical and Extratropical Cyclones Research
  • Meteorological Phenomena and Simulations
  • Oceanographic and Atmospheric Processes
  • Hydrology and Drought Analysis
  • Sugarcane Cultivation and Processing
  • Climate change impacts on agriculture
  • Marine and coastal ecosystems
  • Atmospheric chemistry and aerosols
  • Geological and Geophysical Studies
  • Atmospheric and Environmental Gas Dynamics
  • Geological and Tectonic Studies in Latin America
  • Ocean Waves and Remote Sensing
  • Blind Source Separation Techniques
  • Atmospheric Ozone and Climate
  • Flood Risk Assessment and Management
  • Neural Networks and Applications
  • Hydrological Forecasting Using AI
  • Spectroscopy and Chemometric Analyses
  • Hydrology and Watershed Management Studies
  • Methane Hydrates and Related Phenomena

George Mason University
2017-2023

APEC Climate Center
2014-2015

Abstract In early 2018, Cape Town (population ~3.7 million) was at risk of being one the first major metropolitan areas in world to run out water. This due a severe multi-year drought that led levels supply dams falling an unprecedented low. Here we analyze rainfall data from city catchment areas, including rare centennial records surrounding region, assess severity 2015–2017 drought. We find there has been long-term decline number winter days, but this trend generally masked by fluctuations...

10.1038/s41612-019-0084-6 article EN cc-by npj Climate and Atmospheric Science 2019-08-08

Abstract The occurrence of boreal winter Rossby wave breaking (RWB) along with the quantitative role synoptic transient eddy momentum and heat fluxes directly associated RWB are examined during development Euro-Atlantic circulation regimes using ERA-Interim. Results compared to those from seasonal reforecasts made Integrated Forecast System model ECWMF coupled NEMO ocean model. both Scandinavian blocking Atlantic ridge is coincident anticyclonic (AWB); however, do not contribute (and, in...

10.1175/jas-d-16-0263.1 article EN other-oa Journal of the Atmospheric Sciences 2017-03-13

Abstract A three-dimensional evolution of Madden–Julian oscillation (MJO) diabatic heating for October–March from satellite data is constructed: the propagates eastward three cycles, modulated by likelihood a given MJO phase to occur on calendar day. This added temperature tendencies each member an ensemble 48 (1 October–31 March) simulations with Community Earth System Model. The leading two most predictable modes planetary wave vertically integrated total (added plus model generated)...

10.1175/jas-d-14-0145.1 article EN other-oa Journal of the Atmospheric Sciences 2014-10-01

Abstract Subtropical anticyclones and midlatitude storm tracks are key components of the large-scale atmospheric circulation. Focusing on Southern Hemisphere, seasonality three dominant subtropical anticyclones, situated over South Pacific, Atlantic, south Indian Ocean basins, has a large influence local weather climate within America, southern Africa, Australia, respectively. Generally speaking, sea level pressure Hemisphere subtropics reaches its seasonal maximum during winter season when...

10.1175/jcli-d-20-0509.1 article EN Journal of Climate 2021-02-01

Bangladesh and northeast India are the most densely populated regions in world where severe floods as a result of extreme rainfall events kill hundreds people cause socio‐economic losses regularly. Owing to local high topography, moisture‐carrying monsoon winds converge near southeast (SEB) (NEBI), which produces significant from May October. Using observed data, we find an increasing trend 1‐day event (150 mmday) frequency during 1950–2021. The quadrupled over western Meghalaya (affecting...

10.1002/qj.4645 article EN cc-by-nc Quarterly Journal of the Royal Meteorological Society 2023-12-22

Abstract Atmospheric rivers (ARs) are examined in a set of aquaplanet simulations using the Model for Prediction Across Scales dynamical core run at multiple horizontal resolutions, namely, 240, 120, and 60 km. As resolution is increased, there an increase occurrence long‐lasting ARs. At same time also local finite‐amplitude wave activity (LWA) upper‐tropospheric absolute vorticity, measure Rossby phase amplitude that closely linked with breaking. Consistent notion changes ARs driven by...

10.1029/2017jd027899 article EN publisher-specific-oa Journal of Geophysical Research Atmospheres 2018-05-16

Abstract Ensemble reforecast experiments are performed for the boreal winters of 2015/16 (an El Niño year) and 2016/17 in order to understand origin highly unexpected low precipitation over Southern California (SoCal) during 2015/16. The specific hypothesis tested is that December–March anomalies (i) SoCal (highly negative) (ii) 200-hPa height field Pacific–North American (PNA) region (unusual an were forced by tropical diabatic heating, as estimated from reanalysis fields. Ten-member...

10.1175/jas-d-19-0064.1 article EN Journal of the Atmospheric Sciences 2019-08-01

Building on the recent advent of concept finite-amplitude wave activity, a contour-following diagnostics for column water vapor (CWV) is developed and applied to pair aquaplanet model simulations understand quantify higher moments in global hydrological cycle. The Lagrangian nature leads more tractable formalism transient, zonally asymmetric component cycle, with strong linear relation emerging between activity precipitation minus evaporation ([Formula: see text]). dry-versus-wet disparity...

10.1175/jcli-d-16-0561.1 article EN other-oa Journal of Climate 2017-02-15

Intervention experiments using the Coupled Forecast System model, version 2 (CFSv2), have been performed in which various Madden-Julian Oscillation (MJO) evolutions were added to model’s internally generated heating: Slow Repeated Cycles, Single Cycle, Fast and Cycle. In each experiment, one of these specified MJO tropical diabatic heating was multiple ensemble reforecasts boreal winter (1 November 31 March for winters: 1980–2010). Since re-forecasts made with identical evolution added,...

10.1080/07055900.2019.1626214 article EN ATMOSPHERE-OCEAN 2019-05-27

Abstract Various multivariate statistical methods exist for analyzing covariance and isolating linear relationships between datasets. The most popular are based on singular value decomposition (SVD) include canonical correlation analysis (CCA), maximum (MCA), redundancy (RDA). In this study, continuum power CCA (CPCCA) is introduced as one extension of regression pairs coupled patterns whose temporal variation maximizes the squared partially whitened variables. Similar to whitening...

10.1175/jcli-d-14-00451.1 article EN other-oa Journal of Climate 2014-10-31

Abstract Recent studies suggest springtime wet extremes and summertime dry will occur more frequently in the U.S. Midwest, potentially leading to devastating agricultural consequences. To understand role of circulation patterns projected changes seasonal precipitation extremes, k -means clustering approach is applied large-ensemble experiments Community Earth System Model, version 2 (CESM2-LE), ensemble projections CMIP6. We identify two key atmospheric that are associated with extremely...

10.1175/jcli-d-22-0245.1 article EN Journal of Climate 2022-12-06

Abstract In a recent study, Saha et al. (2019, https://doi.org/10.1029/2018JD030082 ) examine the correlation between boreal summer seasonal mean rainfall over India and variance as function of subseasonal time scale find that has local maximum (exceeding value 0.6) for synoptic scales (2–5 day periods). They claim these results to be major advancement in understanding monsoon predictability but do not provide clear physical explanation. Here we sensitivity this relationship details analysis...

10.1029/2020jd033037 article EN Journal of Geophysical Research Atmospheres 2020-10-15

Abstract Tropical cyclone (TC) landfalls over the U.S. mid-Atlantic region, which include so-called Sandy-like, or westward-curving, tracks, are among most infrequent along East Coast. However, when these events do occur, resulting economic and societal consequences can be devastating. A recent example is Hurricane Sandy in 2012. Multimodel ensemble seasonal hindcasts conducted with a high-atmospheric-resolution coupled prediction system based on ECMWF operational model (Project Minerva)...

10.1175/mwr-d-19-0107.1 article EN Monthly Weather Review 2019-06-06

Abstract Boreal winter simulations of the Community Atmospheric Model, version 4.0, were carried out using observed sea surface temperature (SST) fields from three El Niño events 1982/83, 1991/92, and 1997/98 [control (CTL) runs] climatology (CLIM run). In each case, 50 ensemble members run (1 November–31 March). The diabatic heating Q at every grid point, level, day CTL runs in Indo-Pacific region was stored used four additional suites experiments, which parallels appropriate suite. suite,...

10.1175/jas-d-14-0162.1 article EN other-oa Journal of the Atmospheric Sciences 2015-02-09

Abstract The Indian summer monsoon is partly modulated by persistent remote forcing from the tropical Indo-Pacific, evident in dominant observed teleconnection patterns, namely, El Niño–Southern Oscillation (ENSO) and equatorial Ocean (EQUINOO). In atmosphere, these teleconnections are presumably driven diabatic heating, primarily associated with release of latent heat condensation rainfall. However, coupled atmosphere–ocean models, biases result large systematic errors heating. This study...

10.1175/jas-d-21-0231.1 article EN Journal of the Atmospheric Sciences 2022-02-14

Based on the experiments with Coupled Forecast System version 2 (CFSv2), mechanism by which Madden-Julian Oscillation (MJO) modulates North Atlantic (NAO) is investigated. To isolate cyclic MJO heating an eastward propagation over Indian Ocean and western Pacific, three sets of are conducted spatio-temporal varying added to model’s internally generated heating. The results suggest that anomalous Ocean, rather than dominates formation NAO anomaly in following 10-20 days. triggers a westward...

10.1002/essoar.10504746.1 preprint EN 2020-11-23
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