Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases
Over the last six to seven decades, there has been a substantial increase in atmospheric research to better understand the dynamics and evolution of atmospheric blocking events. It is well known that atmospheric blocking serves as a catalyst for increasing the frequency of atmospheric flow regime st...
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| Format: | Article |
| Language: | English |
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Wiley
2018-01-01
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| Series: | Advances in Meteorology |
| Online Access: | http://dx.doi.org/10.1155/2018/1217830 |
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| author | Jordan L. Rabinowitz Anthony R. Lupo Patrick E. Guinan |
| author_facet | Jordan L. Rabinowitz Anthony R. Lupo Patrick E. Guinan |
| author_sort | Jordan L. Rabinowitz |
| collection | DOAJ |
| description | Over the last six to seven decades, there has been a substantial increase in atmospheric research to better understand the dynamics and evolution of atmospheric blocking events. It is well known that atmospheric blocking serves as a catalyst for increasing the frequency of atmospheric flow regime stagnation and forecast unpredictability. This study built upon the results of previous work by expanding upon the findings of various climatologies and case studies. This work analyzes specific trends observed in association with atmospheric blocking predominantly across the central and eastern Pacific Ocean. Such trends include the relationship between the size, duration, and onset position of atmospheric blocking events and the frequency, duration, and intensity of heavy rainfall events across the central United States. A strong focus is placed on examining the duration and spatial extent of atmospheric blocking which has been found to influence the intensity of heavy rainfall events. The goal is to further bridge the gap between the location and duration of blocking highs and the intensity, duration, and frequency of heavy rainfall events which occur downstream of such blocking events. |
| format | Article |
| id | doaj-art-d9bfacd672224e91a95f8c5d3d2b0118 |
| institution | Kabale University |
| issn | 1687-9309 1687-9317 |
| language | English |
| publishDate | 2018-01-01 |
| publisher | Wiley |
| record_format | Article |
| series | Advances in Meteorology |
| spelling | doaj-art-d9bfacd672224e91a95f8c5d3d2b01182025-02-03T06:48:29ZengWileyAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/12178301217830Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO PhasesJordan L. Rabinowitz0Anthony R. Lupo1Patrick E. Guinan2Atmospheric Sciences Program, School of Natural Resources, University of Missouri, Columbia, MO, USAAtmospheric Sciences Program, School of Natural Resources, University of Missouri, Columbia, MO, USAMissouri Climate Center, College of Agriculture, Food, and Natural Resources, University of Missouri, Columbia, MO 65211, USAOver the last six to seven decades, there has been a substantial increase in atmospheric research to better understand the dynamics and evolution of atmospheric blocking events. It is well known that atmospheric blocking serves as a catalyst for increasing the frequency of atmospheric flow regime stagnation and forecast unpredictability. This study built upon the results of previous work by expanding upon the findings of various climatologies and case studies. This work analyzes specific trends observed in association with atmospheric blocking predominantly across the central and eastern Pacific Ocean. Such trends include the relationship between the size, duration, and onset position of atmospheric blocking events and the frequency, duration, and intensity of heavy rainfall events across the central United States. A strong focus is placed on examining the duration and spatial extent of atmospheric blocking which has been found to influence the intensity of heavy rainfall events. The goal is to further bridge the gap between the location and duration of blocking highs and the intensity, duration, and frequency of heavy rainfall events which occur downstream of such blocking events.http://dx.doi.org/10.1155/2018/1217830 |
| spellingShingle | Jordan L. Rabinowitz Anthony R. Lupo Patrick E. Guinan Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases Advances in Meteorology |
| title | Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases |
| title_full | Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases |
| title_fullStr | Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases |
| title_full_unstemmed | Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases |
| title_short | Evaluating Linkages between Atmospheric Blocking Patterns and Heavy Rainfall Events across the North-Central Mississippi River Valley for Different ENSO Phases |
| title_sort | evaluating linkages between atmospheric blocking patterns and heavy rainfall events across the north central mississippi river valley for different enso phases |
| url | http://dx.doi.org/10.1155/2018/1217830 |
| work_keys_str_mv | AT jordanlrabinowitz evaluatinglinkagesbetweenatmosphericblockingpatternsandheavyrainfalleventsacrossthenorthcentralmississippirivervalleyfordifferentensophases AT anthonyrlupo evaluatinglinkagesbetweenatmosphericblockingpatternsandheavyrainfalleventsacrossthenorthcentralmississippirivervalleyfordifferentensophases AT patrickeguinan evaluatinglinkagesbetweenatmosphericblockingpatternsandheavyrainfalleventsacrossthenorthcentralmississippirivervalleyfordifferentensophases |