Correlations between deep convection and lightning activity on a global scale
Satellite observations of cloud top temperature and lightning flash distribution are used to examine the relationship between deep convection and lightning activity over the tropical regions of the northern and southern hemispheres. In agreement with previous work, the analysis of the results shows...
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| Formato: | Capítulo de libro |
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2010
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| LEADER | 16333caa a22014657a 4500 | ||
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| 008 | 190411s2010 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-77955660598 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Ávila, Eldo Edgardo | |
| 245 | 1 | 0 | |a Correlations between deep convection and lightning activity on a global scale |
| 260 | |c 2010 | ||
| 270 | 1 | 0 | |m Ávila, E.E.; Facultad de Matemática, Astronomía y Física, IFEG, Universidad Nacional de Córdoba, CONICET, Córdoba, Argentina; email: avila@famaf.unc.edu.ar |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a Satellite observations of cloud top temperature and lightning flash distribution are used to examine the relationship between deep convection and lightning activity over the tropical regions of the northern and southern hemispheres. In agreement with previous work, the analysis of the results shows that, in the summer of both hemispheres, the lightning activity in continental deep convective storms is more intense than that in marine deep convective storms by a factor of between 7 and 10. Furthermore, it was observed that on average the daily lightning rate per 1°×1° grid cell for the southern hemisphere (SH) is about 20% greater than that of the northern hemisphere (NH), which can be attributed to a larger fractional cover by deep convective clouds in the SH. By using a set of independent indicators, it is shown that deep convection and lightning activity over land are well correlated (with correlation coefficients of 0.8 and 0.6 for NH and SH, respectively). This suggests the capacity for observations to act as a possible method of monitoring continental deep convective clouds, which play a key role in regulating the Earth's climate. Since lightning can be monitored easily from ground networks and satellites, it could be a useful tool for validating the performance of model convective schemes and for monitoring changes in climate parameters. © 2010 Elsevier Ltd. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional para Investigaciones Científicas y Tecnológicas | ||
| 536 | |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica | ||
| 536 | |a Detalles de la financiación: Secretaría Nacional de Ciencia, Tecnología e Innovación, A0811 | ||
| 536 | |a Detalles de la financiación: Secretaria de Ciencia y Tecnología - Universidad Nacional de Córdoba | ||
| 536 | |a Detalles de la financiación: National Research Foundation | ||
| 536 | |a Detalles de la financiación: Fondo para la Investigación Científica y Tecnológica | ||
| 536 | |a Detalles de la financiación: This work was supported by Secretaría de Ciencia y Tecnología de la Universidad Nacional de Córdoba, Consejo Nacional de Investigaciones Científicas y Tecnológicas (CONICET), Agencia Nacional de Promoción Científica (FONCYT), Secretaría de Ciencia y Tecnología: proyecto bilateral A0811(MINCYT-NRF), and the National Research Foundation (NRF) of South Africa. | ||
| 593 | |a Facultad de Matemática, Astronomía y Física, IFEG, Universidad Nacional de Córdoba, CONICET, Córdoba, Argentina | ||
| 593 | |a Hermanus Magnetic Observatory, Hermanus, South Africa | ||
| 593 | |a Physics Department, University of KwaZulu-Natal, Durban, South Africa | ||
| 593 | |a Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad Nacional de Buenos Aires, Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a ATMOSPHERIC ELECTRICITY |
| 690 | 1 | 0 | |a CONVECTIVE PROCESSES |
| 690 | 1 | 0 | |a LIGHTNING |
| 690 | 1 | 0 | |a CLIMATE PARAMETERS |
| 690 | 1 | 0 | |a CLOUD-TOP TEMPERATURES |
| 690 | 1 | 0 | |a CONVECTIVE PROCESSES |
| 690 | 1 | 0 | |a CONVECTIVE STORMS |
| 690 | 1 | 0 | |a CORRELATION COEFFICIENT |
| 690 | 1 | 0 | |a DEEP CONVECTION |
| 690 | 1 | 0 | |a DEEP CONVECTIVE CLOUDS |
| 690 | 1 | 0 | |a EARTH'S CLIMATE |
| 690 | 1 | 0 | |a FRACTIONAL COVER |
| 690 | 1 | 0 | |a GLOBAL SCALE |
| 690 | 1 | 0 | |a GRID CELLS |
| 690 | 1 | 0 | |a GROUND NETWORKS |
| 690 | 1 | 0 | |a LIGHTNING ACTIVITY |
| 690 | 1 | 0 | |a LIGHTNING FLASHES |
| 690 | 1 | 0 | |a MONITORING CHANGE |
| 690 | 1 | 0 | |a NORTHERN HEMISPHERE |
| 690 | 1 | 0 | |a SATELLITE OBSERVATIONS |
| 690 | 1 | 0 | |a SOUTHERN HEMISPHERE |
| 690 | 1 | 0 | |a TROPICAL REGIONS |
| 690 | 1 | 0 | |a ATMOSPHERIC ELECTRICITY |
| 690 | 1 | 0 | |a ATMOSPHERIC THERMODYNAMICS |
| 690 | 1 | 0 | |a CLIMATE MODELS |
| 690 | 1 | 0 | |a CLOUDS |
| 690 | 1 | 0 | |a EARTH (PLANET) |
| 690 | 1 | 0 | |a LIGHTNING PROTECTION |
| 690 | 1 | 0 | |a NATURAL CONVECTION |
| 690 | 1 | 0 | |a STORMS |
| 690 | 1 | 0 | |a LIGHTNING |
| 700 | 1 | |a Burgesser, Rodrigo Exequiel | |
| 700 | 1 | |a Castellano, Nesvit Edit | |
| 700 | 1 | |a Collier, A.B. | |
| 700 | 1 | |a Compagnucci, R.H. | |
| 700 | 1 | |a Hughes, A.R.W. | |
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