Empirical Orthogonal Function (EOF) analysis of monsoon rainfall and satellite-observed outgoing long-wave radiation for Indian monsoon: a comparative study

2004 ◽  
Vol 85 (4) ◽  
pp. 227-234 ◽  
Author(s):  
C. V. Singh
Keyword(s):  
Comparative Study ◽  
Empirical Orthogonal Function ◽  
Monsoon Rainfall ◽  
Indian Monsoon ◽  
Wave Radiation ◽  
Eof Analysis ◽  
Outgoing Long Wave Radiation ◽  
Orthogonal Function ◽  
Long Wave ◽  
Long Wave Radiation

Anomalous land surface temperature and outgoing long-wave radiation observations prior to earthquakes in India and Romania

2011 ◽  
Vol 59 (1) ◽  
pp. 33-46 ◽  
Author(s):  
Vineeta Rawat ◽  
Arun K. Saraf ◽  
Josodhir Das ◽  
Kanika Sharma ◽  
Yazdana Shujat
Keyword(s):  
Surface Temperature ◽  
Land Surface Temperature ◽  
Land Surface ◽  
Wave Radiation ◽  
Outgoing Long Wave Radiation ◽  
Long Wave ◽  
Long Wave Radiation

Surveillance of Vrancea active seismic region in Romania through time series satellite data

2014 ◽  
Vol 6 (2) ◽  
Author(s):  
Maria Zoran ◽  
Roxana Savastru ◽  
Dan Savastru
Keyword(s):  
Time Series ◽  
Satellite Data ◽  
Land Surface ◽  
Main Shock ◽  
Tectonic Activity ◽  
Wave Radiation ◽  
Outgoing Long Wave Radiation ◽  
Seismic Region ◽  
Long Wave ◽  
Long Wave Radiation

AbstractCumulative stress energy in active seismic regions caused by tectonic forces creates various earthquake precursors. This energy transformation may result in enhanced transient thermal infrared (TIR) emission, which can be detected through satellites equipped with thermal sensors like MODIS (Terra/Aqua) and AVHRR (NOAA). Satellite time-series data, coupled with ground based observations, where available, can enable scientists to survey pre-earthquake signals in the areas of strong tectonic activity. This paper presents observations made using time series MODIS and NOAA-AVHRR satellite data for derived multi-parameters including land surface temperature (LST), outgoing long-wave radiation (OLR), and mean air temperature (AT) for the moderate, 5.9 magnitude earthquake, which took place on the 27th of October, 2004, inthe seismic region of Vrancea, in Romania. Anomalous thermal infrared signals, reflected by a rise of several degrees celsius (°C) in LSTs, and higher OLR values were seen several days before the earthquake. AT values in the epicentral area also increased almost two days prior to the earthquake and intensified three days after the main shock. Increases in LSTs and OLR disappeared three days after the main shock. The survey and joint analysis of geospatial and in-situ geophysical information on land surface temperatures and outgoing long-wave radiation provides new insights into the field of seismic hazard assessment in Vrancea, a significant area of tectonic activity in Romania and Europe.

Diurnal variation of the outgoing long-wave radiation: as revealed by the E.R.B.E.

1993 ◽  
Vol 45 (1) ◽  
pp. 1-14 ◽  
Author(s):  
Chandrasekhara R. Kondragunta ◽  
H. Lee Kyle ◽  
Ann T. Mecherikunnel
Keyword(s):  
Diurnal Variation ◽  
Wave Radiation ◽  
Outgoing Long Wave Radiation ◽  
Long Wave ◽  
Long Wave Radiation

Outgoing Long-wave Radiation from Indian Stations

Nature ◽  
1965 ◽  
Vol 207 (4999) ◽  
pp. 852-853 ◽  
Author(s):  
M. G. GUPTA
Keyword(s):  
Wave Radiation ◽  
Outgoing Long Wave Radiation ◽  
Long Wave ◽  
Long Wave Radiation

scholarly journals Understanding the variability of clear-sky outgoing long-wave radiation based on ship-based temperature and water vapour measurements

2006 ◽  
Vol 132 (621) ◽  
pp. 2675-2691 ◽  
Author(s):  
V. O. John ◽  
S. A. Buehler ◽  
A. von Engeln ◽  
P. Eriksson ◽  
T. Kuhn ◽  
...  
Keyword(s):  
Water Vapour ◽  
Wave Radiation ◽  
Outgoing Long Wave Radiation ◽  
Clear Sky ◽  
Long Wave ◽  
Long Wave Radiation
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