GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Language
Years
  • 1
    Publication Date: 2022-05-26
    Description: Author Posting. © American Meteorological Society, 2009. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Bulletin of the American Meteorological Society 90 (2009):459-480, doi:10.1175/2008BAMS2608.1.
    Description: The Indian Ocean is unique among the three tropical ocean basins in that it is blocked at 25°N by the Asian landmass. Seasonal heating and cooling of the land sets the stage for dramatic monsoon wind reversals, strong ocean–atmosphere interactions, and intense seasonal rains over the Indian subcontinent, Southeast Asia, East Africa, and Australia. Recurrence of these monsoon rains is critical to agricultural production that supports a third of the world's population. The Indian Ocean also remotely influences the evolution of El Niño–Southern Oscillation (ENSO), the North Atlantic Oscillation (NAO), North American weather, and hurricane activity. Despite its importance in the regional and global climate system though, the Indian Ocean is the most poorly observed and least well understood of the three tropical oceans. This article describes the Research Moored Array for African–Asian–Australian Monsoon Analysis and Prediction (RAMA), a new observational network designed to address outstanding scientific questions related to Indian Ocean variability and the monsoons. RAMA is a multinationally supported element of the Indian Ocean Observing System (IndOOS), a combination of complementary satellite and in situ measurement platforms for climate research and forecasting. The article discusses the scientific rationale, design criteria, and implementation of the array. Initial RAMA data are presented to illustrate how they contribute to improved documentation and understanding of phenomena in the region. Applications of the data for societal benefit are also described.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © American Meteorological Society, 2009. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Bulletin of the American Meteorological Society 90 (2009): ES5-ES8, doi:10.1175/2008BAMS2608.2.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2023-06-28
    Description: We carried out two campaign observations over the southwestern coastal land and adjacent sea of Sumatera Island, Indonesia, during November-December 2015 (pre-YMC 2015, hereafter Y15) (49 days) and November 2017-January 2018 (YMC-Sumatra 2017, hereafter Y17) (61 days). We deployed two land observation sites in Bengkulu city on the southwestern coast of Sumatra Island with various kinds of instruments including an X-band dual polarization (DP) and operational C-band Doppler radars, and the R/V Mirai over the coastal sea with a C-band DP radar. Intensive 3-hourly soundings were conducted both over the land and the vessel during both periods. Synoptic conditions during the Y15 (Y17) corresponded to El Niño (La Niña) and large scale cloud areas of active Madden-Julian Oscillation (MJO) passed over Sumatra Island in the about later (former) 10 days of the period, i.e., most of both campaign periods were convectively MJO inactive phases. Rainfall at Bengkulu during Y15 showed clear diurnal variation with active thunderstorms every day (31 days) during the Y15 until MJO active phase onset over Sumatra. Whereas rainfall diurnal variation in Y17 was quite unclear and its peak time was delayed approximately 2 hours than that in Y15 though both periods corresponded to mostly MJO inactive phases. In particular, the thunderstorm during Y17 was quite a few (9 days) and only a short time within an hour. Characteristics that brought different convective activities between two campaign periods, e.g., diurnally developed local winds, atmospheric instabilities, and spatiotemporal variations of radar echo distribution, were analyzed for further discussion.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...