Further case studies of tropical atlantic surface atmospheric and oceanic patterns associated with sub-Saharan drought
Journal Article
·
· Journal of Climate; (United States)
- Univ. of Oklahoma, Norman (United States)
- Illinois State Water Survey, Champaign (United States)
Sub-Saharan West Africa (10[degrees]20[degrees]N) receives rainfall from westward-propagating disturbance lines that have their base within and receive most of their moisture from the low-level, wedge-shaped, southwest monsoonal flow off the tropical Atlantic. This paper identifies the tropical Atlantic surface atmospheric and oceanic patterns that accompany drought in sub-Saharan West Africa. Patterns for the four driest years since 1940 are compared with counterparts for the wettest of the last 20 years and 60-year average fields. The key results for the rainy season of three of the four severe sub-Saharan drought years 1972, 1977, 1984 duplicate those obtained earlier. They include (i) a distinctive basinwide sea surface temperature (SST) anomaly pattern (positive departures to the south of[similar to] 10[degrees]N; negative departures between 10[degrees]- 25[degrees]); (ii) a concomitant southward displacement (relative to the 1911-70 mean) of the zone of maximum SST by 250-500 km; (iii) the North (South) Atlantic subtropical high extending farther (less) equatorward than in the 60-year mean; and (iv) associated southward displacements (by 200-350 km) of the near-equatorial pressure trough, wind direction discontinuity between Northern and Southern hemisphere trades, and zones of maximum rainfall frequency and total cloud amount. Very deficient sub-Saharan rainy seasons tend to coincide with the southwesterly surface monsoonal flow. Only the SST patterns of the aforementioned results show evidence of evolving during preceding seasons. This indicates the potential for tropical Atlantic SST to provide the basis for the prediction of sub-Saharan rainy season quality several months in advance. These results were not characteristic of the other extremely deficient sub-Saharan rainy season investigated (1983) or the nondrought rainy season studied for comparative purposes (1975).
- OSTI ID:
- 6890342
- Journal Information:
- Journal of Climate; (United States), Journal Name: Journal of Climate; (United States) Vol. 5:5; ISSN JLCLEL; ISSN 0894-8755
- Country of Publication:
- United States
- Language:
- English
Similar Records
Spatiotemporal variability of west African rainfall. Part II. Associated surface and airmass characteristics
Linkages of Remote Sea Surface Temperatures and Atlantic Tropical Cyclone Activity Mediated by the African Monsoon
Linkages of remote sea surface temperatures and Atlantic tropical cyclone activity mediated by the African monsoon
Journal Article
·
Fri May 01 00:00:00 EDT 1992
· Journal of Climate; (United States)
·
OSTI ID:6890330
Linkages of Remote Sea Surface Temperatures and Atlantic Tropical Cyclone Activity Mediated by the African Monsoon
Journal Article
·
Tue Jan 27 23:00:00 EST 2015
· Geophysical Research Letters, 42(2):572-578
·
OSTI ID:1184958
Linkages of remote sea surface temperatures and Atlantic tropical cyclone activity mediated by the African monsoon
Journal Article
·
Mon Jan 19 19:00:00 EST 2015
· Geophysical Research Letters
·
OSTI ID:1402368
Related Subjects
54 ENVIRONMENTAL SCIENCES
540110*
AFRICA
AIR
ANNUAL VARIATIONS
ATLANTIC OCEAN
ATMOSPHERIC CIRCULATION
ATMOSPHERIC PRECIPITATIONS
ATMOSPHERIC PRESSURE
DISASTERS
DROUGHTS
EARTH PLANET
FLUIDS
FORECASTING
GASES
MOISTURE
MONITORING
MONSOONS
OCEANIC CIRCULATION
PLANETS
RAIN
SEAS
SEASONAL VARIATIONS
SOUTHERN HEMISPHERE
STORMS
SURFACE AIR
SURFACE WATERS
TEMPERATURE MONITORING
TROPICAL REGIONS
VARIATIONS
WIND
540110*
AFRICA
AIR
ANNUAL VARIATIONS
ATLANTIC OCEAN
ATMOSPHERIC CIRCULATION
ATMOSPHERIC PRECIPITATIONS
ATMOSPHERIC PRESSURE
DISASTERS
DROUGHTS
EARTH PLANET
FLUIDS
FORECASTING
GASES
MOISTURE
MONITORING
MONSOONS
OCEANIC CIRCULATION
PLANETS
RAIN
SEAS
SEASONAL VARIATIONS
SOUTHERN HEMISPHERE
STORMS
SURFACE AIR
SURFACE WATERS
TEMPERATURE MONITORING
TROPICAL REGIONS
VARIATIONS
WIND