Abstract

Precipitation events are infrequent in the dry quarter (SON) of the Alcântara Launch Center (Centro de Lançamento de Alcântara, CLA), the main launch site of the Brazilian Space Program. However, their occurrence could be a risk for activities during launch missions. In this work, the observational features of wet days (daily precipitation total ≥ 1 mm/day) in the dry quarter of the CLA region were studied. Daily precipitation totals over the course of 37 years (1979-2016, except 2006), outgoing longwave radiation (OLR) data and ERA-Interim reanalysis data were used. On average, in the dry quarter, there were 9 wet days, which accumulated 32 mm. The number and quarterly precipitation total of wet days showed pronounced interannual variability. This variability was negatively and significantly correlated with the interhemispheric sea surface temperature anomalies gradient in the Atlantic Ocean and the wind speed at 925 hPa over the CLA region. Based on a theoretical distribution (log-normal), the probability of occurrence of heavy precipitation days (daily total ≥ 10 mm/day) was only 0.5%. For days with heavy precipitation and deep convection (OLR ≤ 230 W·m-2), over a large area along the northeastern coast of South America including the CLA region, negative OLR differences (from the mean) and the strengthening of favorable conditions for deep convection were found. The large-scale organization of the convective activity and atmospheric features for higher precipitation events obtained in this work could be helpful for nowcasting and short-range weather forecasting during launch missions at the CLA.

Highlights

  • The Alcântara Launch Center (Centro de Lançamento de Alcântara, CLA), located on the northern coast of Brazil (NCB), is the main launch site of the Brazilian Space Program (Fig. 1a)

  • Statistics of number of wet days (NWET) and PWET for the dry quarter in CLA are shown in Tab average in the dry quarter, from the mean values, there are 9 wet days, which accum mm

  • Further studies are needed to determine other factors that could explain the variability of PWET and NWET beyond gradient in the Atlantic Ocean (GRAD) and MAG

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Summary

Introduction

The Alcântara Launch Center (Centro de Lançamento de Alcântara, CLA), located on the northern coast of Brazil (NCB), is the main launch site of the Brazilian Space Program (Fig. 1a). The ideal conditions for activities at CLA, when the aerospace vehicle or its parts are outside the tower shelter (Torre Móvel de Integração) and directly exposed to surface atmospheric conditions, include the absence of precipitation, lightning and strong surface winds (Marques and Fisch 2005). In the dry quarter of CLA, which corresponds to the austral spring (September to November, SON), the limiting factor for these activities, including the determination of the launch window, is usually the presence of strong surface winds. In this quarter the average surface wind speed is higher and precipitation events are infrequent (Pereira et al 2002; Barros 2008). In the launch missions called Operação Maracati II (VSB-30; 16 Nov to 14 Dec 2010) (Souza 2011) and Operação

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