1029:
1162:. These clouds have been found to be present more often than expected in common stratocumulus layers. These clouds are persistent year-round off the coast, but are only drawn inland during June Gloom events and related phenomena elsewhere in the world. Observations suggest that when marine stratus is present alone, drizzle is minimized. However, scientists believe that the presence of actinoform clouds within the marine stratus is indicative of an increase in drizzle and the onset of precipitation. Observation and computer modeling have shown that the shape of the cloud fields actually rearrange themselves when the clouds start to rain.
40:
1143:
1059:, which flows out of the cold Gulf of Alaska, enhances the contrast between the cool air below the inversion layer and the warm air above it. A stronger inversion layer – one with a greater difference in temperature between the air above and the air below – often results in more and deeper marine layer clouds that persist longer into the day. Upwelling of colder-than-normal ocean water, associated with a
114:
1040:. When the relative humidity reaches 100%, the water vapor condenses into liquid water droplets and the clouds begin to form. The stable top of the marine layer, a result of the temperature inversion, prevents any dry, warm air from above the inversion from mixing with the stratus deck. This confines the stratus deck to a relatively narrow vertical band in the atmosphere, allowing it to strengthen.
1013:
1021:
153:, move in at night, usually after midnight, and typically dissipate in the late morning, giving way to clear, sunny skies. During a heavy June Gloom season, the condition may persist into the afternoon, or even all day during an exceptionally strong event. Often, the air is saturated with moisture, and
1070:
the clouds over the coastal lands. The extent of inland advection is limited by southern
California's coastal mountain ranges. The winds will continue to push the cloud layer onshore until they encounter mountains at or above the altitude of the clouds themselves, with the mountains then preventing
1035:
The low-altitude stratus clouds that make up the June Gloom cloud layer form over the nearby ocean, and are transported over the coastal areas by the region's prevailing westerly winds. The sheet-like stratus clouds are almost uniformly horizontal, covering large areas but having relatively shallow
1003:
The negative effects of a long June Gloom on the coastal
California tourism industry is often reported in the local news media. The phenomenon can be especially disorienting to visitors from inland areas who, coming from the summer heat, would not expect cool temperatures and clouds and fog at the
1074:
The marine layer clouds of a June Gloom day usually are at their maximum at dawn, when the surface air is at a minimum temperature and the temperature difference in the inversion layer is at its maximum. The air beneath the inversion base being at its coolest also makes it likely that it will be
117:
Satellite image of a strong June Gloom day, showing marine layer clouds covering the coastal regions of the counties of Santa
Barbara, Ventura, Los Angeles, Orange, and San Diego. The San Fernando Valley and San Gabriel Valley also are covered, with clouds spilling inland as far eastward as San
1093:
is in place over the region, and the marine layer will be very weak or nonexistent when there is a strong high-pressure system affecting southern
California. The National Weather Service graphic on the right explains the effects of atmospheric conditions upon the marine layer and local weather
168:
By late morning to early afternoon, solar heating usually is sufficient to evaporate the clouds, and the sun emerges. The phenomenon forms earliest and lasts longest at the coast, with weaker effects as it moves further inland. When the marine layer is strong and deep, clouds can fill the
1082:, which is caused by the temperature and pressure difference between warm areas inland and the cool air over the ocean, often develops on warm summer days as well, increasing the on-shore flow pattern and maintaining a constant flow of marine stratus clouds onto the coastal areas.
225:
The months of May and June are typically the cloudiest months of the year in coastal southern
California, having only 59% and 58% sunny days, respectively, on average in San Diego. The number of days in May and June that are "gloomy" varies from year to year. Anomalies in
105:. This weather pattern is relatively rare, and occurs only in a few other parts of the world where climates and conditions are similar. Scientists study the cloud fields that make up June Gloom to increase understanding of cloud behavior at the onset of precipitation.
1233:
and from
November 1871 to June 1939 and a variety of buildings at downtown, and at San Diego Int'l (Lindbergh Field) since July 1939. Temperature records, however, only date from October 1874. For more information on data coverage, see
992:, although this is not well-supported by evidence. However, the normally-very-sunny Los Angeles climate also is home to people who thrive during the brief seasonal respite the gloom provides from the unending sunshine and clear skies.
1036:
depth of 500 to 2,000 metres (1,600 to 6,600 ft). These clouds begin to form when wind mixes moisture from the ocean surface into the air. The air cools and expands as it is mixed and moves upward, and this cooling increases the
205:
A combination of atmospheric and oceanic conditions must be just right in order for June Gloom to form, and these conditions usually align only around May and June of each year. These include the marine layer effect common to the
1051:-pressure system (which is strongest during the summer) meets with the rising, cooling air from the sea surface, producing a very stable layer of air that caps the cool air from rising any further. The strength of this
1071:
any further inland progress of the marine layer. The foothill regions of these mountains experience some of the thickest fog and drizzle, as they are essentially in the clouds at this point.
197:
and plunge into a cloudy, fog-filled Los
Angeles. On a weak June Gloom morning, the clouds and fog may only be present within a mile or two of the coastline, affecting only the beach cities.
130:
clouds covering the coast of southern
California, extending a varying distance inland depending on the strength of the June Gloom effect that day. On a strong June Gloom day, the clouds and
189:
on exceptionally strong June Gloom mornings. If conditions are not as strong, the Basin may be filled while the valleys may be clear. It is not uncommon for motorists to drive over the
1537:
1445:
1158:
Researchers have discovered that the cloud fields forming June Gloom and related phenomena from other west-coast marine-influenced climates are excellent places to find and study
1441:
1220:
Mean monthly maxima and minima (i.e. the highest and lowest temperature readings during an entire month or year) calculated based on data at said location from 1981 to 2010.
66:
skies with cool temperatures during the late spring and early summer. While it is most common in the month of June, it can occur in surrounding months, giving rise to other
1516:
1471:
1420:
1559:
97:, and gives way to sunny skies. May and June together are usually the cloudiest months in coastal California. June Gloom is stronger in years associated with a
1729:
1467:
1114:
clouds, other locations matching the daily and seasonal effects of
Southern California's June Gloom are relatively rare. These include the western coast of
1089:
passing over southern
California will produce the deepest and most extensive June Gloom marine layer. The marine layer effect is weakened when a weak
230:
can be used to forecast the length and intensity of the June Gloom phenomenon in a given season. Years with warmer ocean temperatures, referred to as
1495:
1028:
1229:
Official precipitation records for San Diego were kept at the Weather Bureau Office in downtown from October 1850 to December 1859 at the
1305:
1272:
1055:
affects the strength of the marine layer, and how long it will take the clouds to dissipate. Additionally, the cool ocean water of the
1024:
A weak, shallow layer of clouds hovering over the coast of California, typical of the dissipation of the marine layer later in the day.
255:
165:. Fog and drizzle normally are found near the furthest inland extent of the gloom, where the cloud deck is closest to the ground.
89:, though usually not rain. June Gloom usually clears up between mid-morning and early afternoon, depending on the strength of the
1016:
A very well-formed and distinct Catalina eddy directly west of San Diego. The marine layer clouds over the land have dissipated.
1368:
1060:
625:
235:
231:
207:
102:
1714:
1047:
is crucial to the formation of the marine stratus that produce June Gloom. Compression and warming of air sinking out of the
1404:
1724:
39:
1615:
989:
1301:
1342:
1142:
1186:
1052:
1044:
227:
211:
1672:
1176:
1588:
1704:
249:
for the months of May and June, which are the two months when the June Gloom pattern is the strongest.
146:
of southern California. It's not uncommon for the layer to persist into the mid-afternoon or evening.
1393:
1191:
1181:
1090:
259:
182:
1492:
1086:
194:
174:
55:
1641:
218:, and sufficiently cool ocean water off the coast. The June Gloom pattern is also enhanced by the
1056:
1048:
178:
139:
75:
1262:
1260:
1258:
1256:
1254:
1230:
1196:
1151:
1037:
935:
888:
569:
522:
215:
170:
131:
33:
70:, such as “Graypril,” “May Gray,” “No-Sky July,” “Fogust”, and “Summer Bummer”. Low-altitude
1159:
234:, may result in fewer gray days in May and June. Cooler ocean temperatures, associated with
1499:
1502:. Climate Database Modernization Program, NOAA's National Climatic Data Center. pp. 7–8.
988:
June Gloom has been reported by some Californians to bring on symptoms consistent with
190:
135:
67:
1719:
1698:
1667:
1512:
1416:
1335:
1111:
1107:
219:
186:
143:
127:
119:
94:
71:
1709:
1268:
1103:
150:
113:
90:
1119:
59:
1584:
1079:
98:
44:
1067:
1012:
1309:
1300:
California Nevada Applications Program/California Climate Change Center.
1201:
1127:
63:
17:
1131:
1123:
162:
86:
1020:
999:
A long June Gloom season, extending late into the summer, is known as
995:
In the early 20th century, this phenomenon was sometimes known as the
1171:
1147:
1141:
1027:
1019:
1011:
112:
38:
1444:. National Oceanic and Atmospheric Administration. Archived from
1066:
Once this marine layer has formed, the prevailing westerly winds
1677:
1339:
1235:
1115:
158:
78:, and spread overnight into the coastal regions of California.
1493:
History of weather observations San Diego, California 1849–1948
1369:"Why does 'June Gloom' typically come only this time of year?"
154:
82:
1661:
1659:
1560:"San Diego/Lindbergh Field CA Climate Normals 1961–1990"
1102:
While many parts of the world commonly have an offshore
1614:
Victoria Clayton, Special to The Times (May 28, 2007).
1579:
1577:
1616:"For some, too much sunshine may bring on the blues"
1540:. National Oceanic & Atmospheric Administration
981:Source: NOAA (sun and relative humidity 1961–1990)
214:caused by subsidence of high-pressure air from the
1329:
1327:
241:The climate charts below show a clear drop in the
1562:. National Oceanic and Atmospheric Administration
1375:. Southern California Public Radio. June 11, 2014
134:, penetrate far inland down valleys such as the
126:A typical June Gloom morning consists of marine
1517:National Oceanic and Atmospheric Administration
1472:National Oceanic and Atmospheric Administration
1421:National Oceanic and Atmospheric Administration
1442:"Station Name: CA LOS ANGELES DWTN USC CAMPUS"
1295:
1293:
1291:
1289:
101:, and weaker or nonexistent in years with an
8:
1075:saturated with a relative humidity of 100%.
262:), 1981–2010 normals, extremes 1877–present
81:The overcast skies often are accompanied by
628:(1981–2010 normals, extremes 1874–present)
58:term for a weather pattern that results in
1538:"Station Name: CA San Diego Lindbergh FLD"
93:and the distance of the location from the
157:also develops, along with frequent light
1138:Actinoform clouds and drizzle prediction
1063:, can strengthen this effect even more.
622:
252:
132:fog may cover the San Francisco Bay Area
27:Weather phenomenon in coastal California
1250:
1213:
238:, usually foretell a more gray period.
1363:
1361:
1359:
1098:Similar weather elsewhere in the world
1642:"Voyager: Can May Gray be Predicted?"
1394:San Diego Union Tribune, June 8, 2004
1267:Scripps Institution of Oceanography.
7:
1666:Amanda Leigh Haag (August 9, 2005).
1513:"NowData – NOAA Online Weather Data"
1468:"LOS ANGELES/WBO CA Climate Normals"
1417:"NowData – NOAA Online Weather Data"
1405:San Diego Union Tribune, May 7, 2010
149:The clouds, which are formed by the
43:June Gloom conditions prevailing at
1730:Weather events in the United States
1644:. Scripps Institute of Oceanography
1336:"NWS Jet Stream – The Marine Layer"
1306:University of California, San Diego
1273:Scripps Institution of Oceanography
25:
1668:"Cloudy With a Chance of Drizzle"
32:For the Camila Cabello song, see
1302:"California May Grey/June Gloom"
1146:Actinoform clouds imaged by the
74:form over the cool water of the
208:West Coast of the United States
254:Climate data for Los Angeles (
222:local to southern California.
1:
817:Average rainfall inches (mm)
615:Source: NOAA (sun 1961–1977)
451:Average rainfall inches (mm)
1593:San Diego Magazine – Journal
1094:conditions in more detail.
990:seasonal affective disorder
747:Mean daily minimum °F (°C)
677:Mean daily maximum °F (°C)
381:Mean daily minimum °F (°C)
311:Mean daily maximum °F (°C)
243:mean monthly sunshine hours
122:is visible near the center.
47:in late morning, June 2013.
1746:
1640:Mark M. (April 30, 2014).
1334:National Weather Service.
1269:"Marine Layer Information"
980:
614:
181:, even extending into the
31:
933:
886:
816:
746:
676:
671:
668:
665:
662:
659:
656:
653:
650:
647:
644:
641:
638:
635:
632:
567:
520:
450:
380:
310:
305:
302:
299:
296:
293:
290:
287:
284:
281:
278:
275:
272:
269:
266:
247:percent possible sunshine
1343:National Weather Service
1150:instrument on board the
1122:, the western coasts of
173:and spill over into the
1187:Inversion (meteorology)
626:San Diego Int'l Airport
228:sea surface temperature
1673:NASA Earth Observatory
1177:Climate of Los Angeles
1155:
1032:
1025:
1017:
193:from the clear, sunny
123:
48:
1715:Climate of California
1498:May 25, 2017, at the
1145:
1031:
1023:
1015:
142:, or extend into the
116:
42:
1595:. San Diego Magazine
1192:Marine stratocumulus
1182:Climate of San Diego
1134:in southern Africa.
1120:Macaronesian Islands
1091:high pressure system
1053:subsidence inversion
183:Santa Clarita Valley
1725:Southern California
1087:low pressure system
629:
263:
195:San Fernando Valley
175:San Fernando Valley
56:Southern California
1156:
1057:California Current
1049:North Pacific High
1033:
1026:
1018:
623:
253:
179:San Gabriel Valley
140:central California
124:
76:California Current
49:
1620:Los Angeles Times
1231:Mission San Diego
1197:San Francisco fog
1160:actinoform clouds
1038:relative humidity
985:
984:
936:possible sunshine
624:Climate data for
619:
618:
570:possible sunshine
216:subtropical ridge
210:, an atmospheric
171:Los Angeles Basin
34:June Gloom (song)
16:(Redirected from
1737:
1689:
1688:
1686:
1684:
1663:
1654:
1653:
1651:
1649:
1637:
1631:
1630:
1628:
1626:
1611:
1605:
1604:
1602:
1600:
1581:
1572:
1571:
1569:
1567:
1556:
1550:
1549:
1547:
1545:
1534:
1528:
1527:
1525:
1523:
1509:
1503:
1489:
1483:
1482:
1480:
1478:
1464:
1458:
1457:
1455:
1453:
1438:
1432:
1431:
1429:
1427:
1413:
1407:
1402:
1396:
1391:
1385:
1384:
1382:
1380:
1365:
1354:
1353:
1351:
1349:
1331:
1322:
1321:
1319:
1317:
1312:on June 13, 2010
1308:. Archived from
1297:
1284:
1283:
1281:
1279:
1264:
1238:
1227:
1221:
1218:
630:
264:
21:
1745:
1744:
1740:
1739:
1738:
1736:
1735:
1734:
1695:
1694:
1693:
1692:
1682:
1680:
1665:
1664:
1657:
1647:
1645:
1639:
1638:
1634:
1624:
1622:
1613:
1612:
1608:
1598:
1596:
1583:
1582:
1575:
1565:
1563:
1558:
1557:
1553:
1543:
1541:
1536:
1535:
1531:
1521:
1519:
1511:
1510:
1506:
1500:Wayback Machine
1490:
1486:
1476:
1474:
1466:
1465:
1461:
1451:
1449:
1448:on May 25, 2017
1440:
1439:
1435:
1425:
1423:
1415:
1414:
1410:
1403:
1399:
1392:
1388:
1378:
1376:
1367:
1366:
1357:
1347:
1345:
1333:
1332:
1325:
1315:
1313:
1299:
1298:
1287:
1277:
1275:
1266:
1265:
1252:
1247:
1242:
1241:
1228:
1224:
1219:
1215:
1210:
1168:
1140:
1100:
1045:inversion layer
1010:
986:
881:
876:
871:
866:
861:
856:
851:
846:
841:
836:
831:
826:
821:
811:
806:
801:
796:
791:
786:
781:
776:
771:
766:
761:
756:
751:
741:
736:
731:
726:
721:
716:
711:
706:
701:
696:
691:
686:
681:
620:
515:
510:
505:
500:
495:
490:
485:
480:
475:
470:
465:
460:
455:
445:
440:
435:
430:
425:
420:
415:
410:
405:
400:
395:
390:
385:
375:
370:
365:
360:
355:
350:
345:
340:
335:
330:
325:
320:
315:
203:
201:Climate effects
161:and occasional
111:
37:
28:
23:
22:
15:
12:
11:
5:
1743:
1741:
1733:
1732:
1727:
1722:
1717:
1712:
1707:
1697:
1696:
1691:
1690:
1655:
1632:
1606:
1573:
1551:
1529:
1504:
1491:Conner, Glen.
1484:
1459:
1433:
1408:
1397:
1386:
1355:
1323:
1285:
1249:
1248:
1246:
1243:
1240:
1239:
1222:
1212:
1211:
1209:
1206:
1205:
1204:
1199:
1194:
1189:
1184:
1179:
1174:
1167:
1164:
1139:
1136:
1099:
1096:
1009:
1006:
1001:Summer Bummer.
983:
982:
978:
977:
974:
971:
968:
965:
962:
959:
956:
953:
950:
947:
944:
941:
938:
931:
930:
927:
924:
921:
918:
915:
912:
909:
906:
903:
900:
897:
894:
891:
889:sunshine hours
884:
883:
878:
873:
868:
863:
858:
853:
848:
843:
838:
833:
828:
823:
818:
814:
813:
808:
803:
798:
793:
788:
783:
778:
773:
768:
763:
758:
753:
748:
744:
743:
738:
733:
728:
723:
718:
713:
708:
703:
698:
693:
688:
683:
678:
674:
673:
670:
667:
664:
661:
658:
655:
652:
649:
646:
643:
640:
637:
634:
621:
617:
616:
612:
611:
608:
605:
602:
599:
596:
593:
590:
587:
584:
581:
578:
575:
572:
565:
564:
561:
558:
555:
552:
549:
546:
543:
540:
537:
534:
531:
528:
525:
523:sunshine hours
518:
517:
512:
507:
502:
497:
492:
487:
482:
477:
472:
467:
462:
457:
452:
448:
447:
442:
437:
432:
427:
422:
417:
412:
407:
402:
397:
392:
387:
382:
378:
377:
372:
367:
362:
357:
352:
347:
342:
337:
332:
327:
322:
317:
312:
308:
307:
304:
301:
298:
295:
292:
289:
286:
283:
280:
277:
274:
271:
268:
251:
202:
199:
191:Sepulveda Pass
136:Salinas Valley
118:Bernardino. A
110:
107:
72:stratus clouds
68:colloquialisms
26:
24:
14:
13:
10:
9:
6:
4:
3:
2:
1742:
1731:
1728:
1726:
1723:
1721:
1718:
1716:
1713:
1711:
1708:
1706:
1703:
1702:
1700:
1679:
1675:
1674:
1669:
1662:
1660:
1656:
1643:
1636:
1633:
1625:September 13,
1621:
1617:
1610:
1607:
1594:
1590:
1587:(June 2007).
1586:
1580:
1578:
1574:
1561:
1555:
1552:
1539:
1533:
1530:
1518:
1514:
1508:
1505:
1501:
1497:
1494:
1488:
1485:
1473:
1469:
1463:
1460:
1447:
1443:
1437:
1434:
1422:
1418:
1412:
1409:
1406:
1401:
1398:
1395:
1390:
1387:
1374:
1370:
1364:
1362:
1360:
1356:
1348:September 13,
1344:
1341:
1337:
1330:
1328:
1324:
1311:
1307:
1303:
1296:
1294:
1292:
1290:
1286:
1274:
1270:
1263:
1261:
1259:
1257:
1255:
1251:
1244:
1237:
1232:
1226:
1223:
1217:
1214:
1207:
1203:
1200:
1198:
1195:
1193:
1190:
1188:
1185:
1183:
1180:
1178:
1175:
1173:
1170:
1169:
1165:
1163:
1161:
1153:
1149:
1144:
1137:
1135:
1133:
1129:
1125:
1121:
1117:
1113:
1112:stratocumulus
1109:
1105:
1097:
1095:
1092:
1088:
1083:
1081:
1076:
1072:
1069:
1064:
1062:
1058:
1054:
1050:
1046:
1041:
1039:
1030:
1022:
1014:
1007:
1005:
1002:
998:
993:
991:
979:
975:
972:
969:
966:
963:
960:
957:
954:
951:
948:
945:
942:
939:
937:
932:
928:
925:
922:
919:
916:
913:
910:
907:
904:
901:
898:
895:
892:
890:
887:Mean monthly
885:
879:
874:
869:
864:
859:
854:
849:
844:
839:
834:
829:
824:
819:
815:
809:
804:
799:
794:
789:
784:
779:
774:
769:
764:
759:
754:
749:
745:
739:
734:
729:
724:
719:
714:
709:
704:
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689:
684:
679:
675:
631:
627:
613:
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582:
579:
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562:
559:
556:
553:
550:
547:
544:
541:
538:
535:
532:
529:
526:
524:
521:Mean monthly
519:
513:
508:
503:
498:
493:
488:
483:
478:
473:
468:
463:
458:
453:
449:
443:
438:
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398:
393:
388:
383:
379:
373:
368:
363:
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348:
343:
338:
333:
328:
323:
318:
313:
309:
265:
261:
257:
250:
248:
244:
239:
237:
233:
229:
223:
221:
220:Catalina eddy
217:
213:
209:
200:
198:
196:
192:
188:
187:Inland Empire
184:
180:
176:
172:
166:
164:
160:
156:
152:
147:
145:
144:Inland Empire
141:
137:
133:
129:
121:
120:Catalina eddy
115:
108:
106:
104:
100:
96:
95:Pacific Ocean
92:
88:
84:
79:
77:
73:
69:
65:
61:
57:
53:
46:
41:
35:
30:
19:
1705:Weather lore
1681:. Retrieved
1671:
1646:. Retrieved
1635:
1623:. Retrieved
1619:
1609:
1597:. Retrieved
1592:
1564:. Retrieved
1554:
1542:. Retrieved
1532:
1520:. Retrieved
1507:
1487:
1475:. Retrieved
1462:
1450:. Retrieved
1446:the original
1436:
1424:. Retrieved
1411:
1400:
1389:
1377:. Retrieved
1372:
1346:. Retrieved
1314:. Retrieved
1310:the original
1276:. Retrieved
1225:
1216:
1157:
1104:marine layer
1101:
1084:
1077:
1073:
1065:
1042:
1034:
1000:
996:
994:
987:
246:
242:
240:
224:
204:
167:
151:marine layer
148:
125:
91:marine layer
80:
54:is a mainly
51:
50:
29:
1477:October 20,
109:Description
1699:Categories
1589:"In a Fog"
1585:Ron Donoho
1245:References
1154:satellite.
1080:sea breeze
52:June Gloom
45:Seal Beach
1648:April 26,
1522:April 11,
1379:April 26,
1278:April 15,
1085:A strong
1008:Formation
997:high fog.
516:(379.25)
212:inversion
1496:Archived
1373:scpr.org
1236:ThreadEx
1202:Tule fog
1166:See also
1128:Portugal
934:Percent
929:3,054.6
568:Percent
563:3,254.2
260:Downtown
64:overcast
18:High fog
1566:June 2,
1544:June 2,
1426:June 7,
1132:Namibia
1124:Morocco
1108:stratus
1061:La Niña
1004:beach.
857:(0.51)
852:(0.76)
812:(14.2)
802:(12.0)
797:(15.9)
792:(18.4)
787:(19.3)
782:(18.6)
777:(16.7)
772:(15.2)
767:(13.3)
762:(11.8)
757:(10.4)
742:(20.9)
737:(18.2)
732:(20.6)
727:(22.7)
722:(24.4)
717:(24.7)
712:(23.7)
707:(21.6)
702:(20.3)
697:(19.7)
692:(18.7)
687:(18.3)
682:(18.4)
486:(0.25)
446:(13.2)
436:(11.1)
431:(14.8)
426:(17.3)
421:(17.8)
416:(17.6)
411:(15.7)
406:(13.9)
401:(11.9)
396:(10.6)
376:(24.0)
371:(19.8)
366:(22.7)
361:(25.8)
356:(28.4)
351:(29.1)
346:(28.4)
341:(25.6)
336:(23.6)
331:(22.6)
326:(21.2)
321:(20.3)
316:(20.1)
236:La Niña
232:El Niño
163:drizzle
128:stratus
103:El Niño
99:La Niña
87:drizzle
1683:May 4,
1599:May 4,
1452:May 9,
1316:May 4,
1130:, and
1118:, the
1068:advect
926:231.3
923:230.1
920:243.4
917:253.3
914:295.0
911:304.7
908:242.4
905:250.5
902:276.2
899:261.0
896:227.4
893:239.3
882:(263)
862:(3.8)
847:(1.8)
842:(3.0)
807:(9.1)
752:(9.4)
633:Month
560:219.4
557:217.3
554:255.1
551:278.5
548:349.5
545:364.1
542:275.8
539:276.2
536:303.5
533:267.0
530:222.5
527:225.3
496:(6.1)
491:(1.0)
481:(2.3)
476:(6.6)
441:(8.6)
391:(9.6)
386:(8.8)
267:Month
60:cloudy
1208:Notes
1172:Gloom
1152:Terra
1148:MODIS
880:10.34
877:(39)
872:(26)
867:(14)
837:(20)
832:(46)
827:(58)
822:(50)
672:Year
514:14.93
511:(59)
506:(26)
501:(17)
471:(23)
466:(62)
461:(97)
456:(79)
306:Year
1720:Rain
1685:2012
1678:NASA
1650:2016
1627:2011
1601:2012
1568:2015
1546:2015
1524:2016
1479:2013
1454:2014
1428:2013
1381:2016
1350:2011
1340:NOAA
1318:2012
1280:2013
1126:and
1116:Peru
1043:The
875:1.53
870:1.01
865:0.57
860:0.15
855:0.02
850:0.03
845:0.07
840:0.12
835:0.78
830:1.81
825:2.27
820:1.98
810:57.5
805:48.4
800:53.6
795:60.6
790:65.2
785:66.7
780:65.4
775:62.0
770:59.4
765:55.9
760:53.2
755:50.7
750:49.0
740:69.7
735:64.7
730:69.0
725:72.8
720:75.9
715:76.4
710:74.6
705:70.8
700:68.5
695:67.5
690:65.6
685:65.0
680:65.1
669:Dec
666:Nov
663:Oct
660:Sep
657:Aug
654:Jul
651:Jun
648:May
645:Apr
642:Mar
639:Feb
636:Jan
509:2.33
504:1.04
499:0.66
494:0.24
489:0.04
484:0.01
479:0.09
474:0.26
469:0.91
464:2.43
459:3.80
454:3.12
444:55.7
439:47.5
434:52.0
429:58.7
424:63.1
419:64.1
414:63.6
409:60.3
404:57.1
399:53.5
394:51.0
389:49.3
384:47.8
374:75.2
369:67.7
364:72.8
359:78.5
354:83.1
349:84.4
344:83.1
339:78.1
334:74.5
329:72.7
324:70.2
319:68.6
314:68.2
303:Dec
300:Nov
297:Oct
294:Sep
291:Aug
288:Jul
285:Jun
282:May
279:Apr
276:Mar
273:Feb
270:Jan
245:and
185:and
177:and
159:mist
85:and
1710:Fog
1110:or
1106:of
976:69
973:74
970:73
967:69
964:68
961:71
958:70
955:57
952:58
949:71
946:70
943:74
940:75
610:73
607:71
604:70
601:73
598:75
595:84
592:83
589:64
586:64
583:78
580:72
577:72
574:71
256:USC
155:fog
138:in
83:fog
1701::
1676:.
1670:.
1658:^
1618:.
1591:.
1576:^
1515:.
1470:.
1419:.
1371:.
1358:^
1338:.
1326:^
1304:.
1288:^
1271:.
1253:^
1078:A
258:,
62:,
1687:.
1652:.
1629:.
1603:.
1570:.
1548:.
1526:.
1481:.
1456:.
1430:.
1383:.
1352:.
1320:.
1282:.
36:.
20:)
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