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Ground wave

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116:. The imperfect conductivity of the ground tilts the waves forward, dissipating energy into the ground. The long wavelengths of these signals allow them to diffract over the horizon, but this leads to further losses. Signal strength tends to fall exponentially with distance once the Earth's curvature is significant. Above about 10 kHz, 157:
of the band. High frequency over-the-horizon radar may use groundwave at moderate ranges but skywave at longer distances. Military communications in the very low and low frequency range uses ground wave, especially to reach ships and submarines, as groundwaves at these long wavelengths penetrate well below the sea surface.
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was the first author to accurately describe groundwave mathematically, deriving an equation for field strength over a flat earth. Van der Pol and Bremmer published calculations for a spherical Earth from 1937 to 1939. Later work focused on paths with variable conductivity, the effects of terrain and
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during the day when skywave is absent, and can be useful at high frequencies at short ranges. Uses include navigation signals, low-frequency time signals, longwave radio, and AM radio. The increased effectiveness of groundwave at lower frequencies gives AM radio stations more coverage at the low end
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transmissions between 3 and 30 MHz have more modest groundwave range and groundwave is unimportant above 30 MHz. Surface conductivity affects the propagation of ground waves, with highly conductive surfaces such as sea water providing the best propagation, and dry ground and ice performing
168:, low frequencies and ground-wave propagation. To prevent interference with these services, amateur and experimental transmitters were restricted to the high frequencies (HF), felt to be useless since their ground-wave range was limited. Upon discovery of the other propagation modes possible at 205:
of the ionosphere forms and absorbs lower frequency energy. This prevents skywave propagation from being very effective on mediumwave frequencies in daylight hours. At night, when the D layer dissipates, mediumwave transmissions travel better by skywave. Ground waves
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of ground waves varies, reaching tens of meters at medium frequencies over dry ground and even more at lower frequencies. Propagation predictions thus require knowing the electrical properties of subsurface layers, which are best measured from groundwave attenuation.
298:. Naval Electrical Engineering Training, Module 10. Naval Education and Training Professional Development and Technology Center. September 1998. p. 2.16. NavEdTra 14182. Archived from 176:
frequencies, the advantages of HF for commercial and military purposes became apparent. Amateur experimentation was then confined to only authorized frequencies in the range.
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Ground wave is important for radio signals below 30 MHz, but is generally insignificant at higher frequencies where line-of-sight propagation dominates.
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and higher over water when seas are rough. Hills, mountains, urban areas, and forests can create areas of reduced signal strength. The
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but changes in the ground can cause variation in signal strength. Attenuation over land is lowest in the winter in
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Angulo I, Barclay L, Chernov Y, Deminco N, Fernández I, Gil U, Guerra D, Milsom J, Peña I, De la Vega D (2014).
164:, ground waves were used extensively. Early commercial and professional radio services relied exclusively on 53:, because ground waves in radio propagation are not confined to the surface. Groundwave contrasts with 101: 54: 201:
reflect off the ionosphere at night, which is known as skywave. During daylight hours, the lower
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radio communication is via groundwave propagation. Groundwave is also the primary mode for
121: 104:, below 3 MHz, travel efficiently as ground waves. As losses increase with frequency, 317: 8: 89: 161: 113: 92:, with lower frequencies and higher ground conductivity permitting longer distances. 264: 132: 30: 332: 153: 34: 65: 105: 85: 370: 149: 20: 124:
waves travel well; horizontally polarized signals are heavily attenuated.
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As the distance increases, ground waves spread out according to the
318:"Propagation and excitation of surface waves in an absorbing layer" 69: 296:
Introduction to Wave Propagation, Transmission Lines, and Antennas
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communications all make use of it. Range depends on frequency and
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around the Earth's curvature. This radiation is also known as the
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Ling, R. T.; Scholler, J. D.; Ufimtsev, P. Ya. (1998).
315: 368: 16:Radio wave propagating along the Earth's surface 189:objects on the ground, and computer modeling. 127:Groundwave signals are relatively immune to 120:helps bend waves downward. Only vertically 336: 72:broadcasting, navigation systems such as 19:For broader coverage of this topic, see 369: 261:International Telecommunications Union 325:Progress in Electromagnetics Research 245: 243: 241: 239: 237: 235: 233: 231: 253:Handbook on Ground Wave Propagation 13: 14: 388: 228: 323:. Northrop Grumman Corporation. 192: 348:from the original on 2022-10-09 143: 309: 292:"Chapter 2: Ground Waves" 284: 1: 221: 57:that requires no medium, and 7: 377:Radio frequency propagation 179: 95: 10: 393: 18: 55:line-of-sight propagation 259:. Geneva, Switzerland: 82:non-directional beacons 49:, or more properly the 303:(PDF (archive zipped)) 118:atmospheric refraction 37:traveling through the 61:via the ionosphere. 338:10.2528/PIER97071800 162:development of radio 90:ground conductivity 47:Norton surface wave 154:medium frequencies 133:temperate climates 114:inverse-square law 84:, and short-range 51:Norton ground wave 270:978-92-61-18661-6 137:penetration depth 33:that consists of 31:radio propagation 384: 357: 356: 354: 353: 347: 340: 322: 313: 307: 306: 304: 288: 282: 281: 279: 277: 258: 247: 100:Lower frequency 76:, low-frequency 392: 391: 387: 386: 385: 383: 382: 381: 367: 366: 361: 360: 351: 349: 345: 320: 314: 310: 302: 290: 289: 285: 275: 273: 271: 256: 248: 229: 224: 197:Mediumwave and 195: 182: 146: 98: 24: 17: 12: 11: 5: 390: 380: 379: 365: 364: 359: 358: 308: 305:on 2018-05-11. 283: 269: 226: 225: 223: 220: 194: 191: 184:In the 1930s, 181: 178: 145: 142: 106:high frequency 97: 94: 15: 9: 6: 4: 3: 2: 389: 378: 375: 374: 372: 363: 362: 344: 339: 334: 330: 326: 319: 312: 301: 297: 293: 287: 272: 266: 262: 255: 254: 246: 244: 242: 240: 238: 236: 234: 232: 227: 219: 217: 213: 209: 204: 200: 193:Related terms 190: 187: 186:Alfred Norton 177: 175: 171: 167: 163: 158: 155: 151: 150:low-frequency 141: 138: 134: 130: 125: 123: 119: 115: 110: 107: 103: 93: 91: 87: 83: 79: 75: 71: 67: 62: 60: 56: 52: 48: 44: 40: 36: 32: 29:is a mode of 28: 22: 350:. Retrieved 328: 324: 311: 300:the original 295: 286: 274:. Retrieved 252: 216:tropospheric 207: 196: 183: 159: 147: 144:Applications 126: 111: 99: 78:time signals 63: 50: 46: 26: 25: 21:Surface wave 212:ionospheric 170:medium wave 109:the worst. 102:radio waves 43:diffracting 27:Ground wave 352:2018-05-10 222:References 174:short wave 331:: 49–91. 199:shortwave 166:long wave 122:polarized 371:Category 343:Archived 210:include 180:Modeling 96:Overview 70:longwave 35:currents 276:23 July 203:D layer 160:In the 59:skywave 267:  218:waves 208:do not 129:fading 346:(PDF) 321:(PDF) 257:(PDF) 148:Most 74:LORAN 39:earth 278:2024 265:ISBN 214:and 172:and 68:and 333:doi 373:: 341:. 329:19 327:. 294:. 263:. 230:^ 86:HF 80:, 66:AM 355:. 335:: 280:. 23:.

Index

Surface wave
radio propagation
currents
earth
diffracting
line-of-sight propagation
skywave
AM
longwave
LORAN
time signals
non-directional beacons
HF
ground conductivity
radio waves
high frequency
inverse-square law
atmospheric refraction
polarized
fading
temperate climates
penetration depth
low-frequency
medium frequencies
development of radio
long wave
medium wave
short wave
Alfred Norton
shortwave

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