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D 301.45/39:301
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Error analysis of the 10-g, 30-g, and 100-g balloon height tables / |
1 |
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D 301.45/39:302
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On the application of air-coupled seismic waves / |
1 |
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D 301.45/39:303
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Strong wind and vertical wind shear above 30 km / |
1 |
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D 301.45/39:304
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The Variation of the upper atmospheric scale height and its effect on atmospheric tidal wavelenghts / |
1 |
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D 301.45/39:305
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World frequency of high temperature / |
1 |
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D 301.45/39:306
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Study of the diurnal variations of the 5577 A [OI] airglow emission at selected IGY stations / |
1 |
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D 301.45/39:307
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Constructing solar flare events by computer / |
1 |
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D 301.45/39:308
|
Interpretation and application of Nimbus high-resolution infrared radiometer data for Southeast Asia / |
1 |
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D 301.45/39:309
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Graphs of the solar depression angle from 0 to 32 vs. local hour angle for latitudes 0 to 90 / |
1 |
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D 301.45/39:310
|
Nonlinear oscillations of a Maxwellian plasma / |
1 |
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D 301.45/39:311
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Investigation of layered tropospheric structures using forward-scatter techniques / |
1 |
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D 301.45/39:312
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Extreme values of ozone observed in the AFCRL ozonesonde network / |
1 |
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D 301.45/39:313
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Solar elevation, depression and azimuth graphs / |
1 |
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D 301.45/39:314
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On water cluster ions in the ionospheric D region / |
1 |
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D 301.45/39:315
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Improvement of the GEOS-1 North American tracking network from multiple short arc geodetic adjustments / |
1 |
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D 301.45/39:316
|
Estimated frequency of cold temperatures over the northern hemisphere / |
1 |
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D 301.45/39:317
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Pulse sounding with closely spaced receivers as a tool for measuring atmospheric motions and fine structure in the ionosphere : III. the application of the generalized correlation and cross spectral analysis to the model on turbulent drift / |
1 |
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D 301.45/39:318
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Vertical-attenuation model with eight surface meteorological ranges 2 to 13 kilometers / |
1 |
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D 301.45/39:319
|
Microwave spectral observations of coronal condensations / |
1 |
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D 301.45/39:320
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Response of the transition region to infalling material associated with solar flares / |
1 |
