This file was created by scanning the printed publication. Errors identified by the software have been corrected; however, some errors may remain. injury to Plants from Rapidly Dropping !•. Daubenmire Professor of botany, Temperature in Washington and State College of Washington, Northern Idaho Pullman

Ix •ARL¾ 70 years of recorded weather history, Washington and I0 PRIEST RIVER E. E northern Idaho have on three occa- IDAHO sions experienced exceptionally 5 sharp freezes in late autumn or early winter that caused consider- able damage to plants. A brief review of these events is warranted since the records are consistent enough to permit the drawing of -5 significant conclusions.

Freeze of December 1924 -I0 Aside from the actual records of daily maximal and minimal tem- -15 peratures for the freeze of Decem- ber 1924, two publications have re- ferred to its effects on plant li•e. -20 The monthly weather summaryfor Washington (7) indicated damage to .cropsover a wide area, stating -25 that there was suspectedinjury to winter wheat, truck crops, and peach spurs. On the west side of -50 the Cascadesin Washington it is possible that even native taxa were damaged. for the summary also states: "Shrubbery in the Puget Sound country is reported as dam- aged by the cold." Unfortunately the brevity of this comment robs it of mostof its fundamentalbiologic significance,for there is no i•dica- tion as to whether or not the dam- 5- age was confined to exotic "shrub- bery." In the period 1911-1917 a series of plantingsof differentgeographic races of Pinus ponderosa were -5 made at the Priest River Experi- mental Forest in Bonner County, •daho (12). Included were -I0 tions obtained from the Siskiyou and Shasta National Forests which are situated in the mild oceanic -15 climates of southwesternOregon and north central California, re- l•xo. 1.--Diurnal ranges of temperature during the unseasonal cold weather of De- spectively. The sudden drop in cember14-28, 1924. Dashesre•resent smoothedtrend lines based on monthly means, intended to approximate the average ranges of diurnal temperatures at this time temperature (Fig. 1, upper part) of year. Shading of columnsindicates temperatures below the freezing point of on December 15, 1924, when the water. 582 JO•SR•ALOr FORESTRY

Siskiyou planting was eight years er regions, all with more continen- this cold wave that is also charac- old and the Shasta nine years old, tal climatesbut from placesas re- teristic of most others discussedin proved disastrous. Most trees of mote from the test location as Ari- this report is that immediately the Siskiyou planting were killed, zona and South Dakota, withstood prior to the invasion of cold air and the Shasta planting was com- the temperature drop without evi- there was a brief period of abnor- pletely destroyed. Races from oth- dent injury. A curious feaure of mally high temperatures which served to a.ccentuate the extent of the subsequentprecipitous drop. 20 Comparison of the actual tem- _ ,• MOSCOW, IDA. peratures with norms for the sea- 15 son(Fig. 1) doesnot suggestgreat- er abnormality for the coastal re- gion (as exemplifiedby Centralia) IO than for the inlandstation; yet if nativeplants sustained damage, it was confinedto the coastalregion. 5 Freeze of October- 1935 O, In the autumnof 1935,tempera- tures prior to October 17 had not dropped lower than 30øF. in the -5- Weather Bureau instrument shel- ter at Moscow,Idaho (Fig. 2, up- per part). On the 25th, and espe- ciallyon the 26thand 27th,daily c• -Io maximal temperaturesrose well in excessof the average, then on the • -I.5, 28th a massof cold air beganto invadethe area and temperatures droppedrapidly. For a periodof z -20 five consecutivedays temperatures wereso abnormallylow that daily maximal remained below the nor- mal minimalvalues for this season, 15- I-1PULLMAN, WASH.resulting in a condition of about equal intensity but shorter dura- ..... n-nH NOV.6-ZO, 1955 tion than that which destroyed pines at the Priest River Experi- mental Forest 11 years earlier (compareFig. 1, upper half, and Fig. 2, upper half). HUH__...... Commentspublished in the then- current issues of Climatological -$ Data '(8) recognizedthis as "un- usually coldweather for soearly in the season,"resulting in the cold- ø...... /...... I est November temperature since 1893. Elsewhere (9) it was stated that "damage from the early No- -15 vember freeze was considerable" also in Washington, especially to "pears in the Kennewick section, -20 sweet cherry, apricot, and English walnut trees." In the memory of _,o the writer, damageto sweetcherries -?_5 (probably mostly the Lambert va- riety) proved so extensive in the Pullman-Moscow area that many F•o. 2.--Comparison of damaging cold waves for the same area at intervals of 20 trees were cut down the following years. Moscowand Pullman are locatedabout 10 milesapart on similar topography. summer. AUOUST1957 583

Freeze of November 1955 There appeared to be a correla- then when the cold air moved in Almost exactly 20 years later tion between the degree of injury "maximum temperatures remained than the epis•)dedescribed above, and degree of age of plant and below freezing for approximately the weather phenomenon was re- seasonal maturity of leaves. A four days or longer. This was as peated. Both the maximal and young apricot tree (budded to many days with a maximum tem- minimal temperatures were well Tilton and Royal varieties) was perature below freezing as is usual- above normal the day before an in- killed while an established tree ly recorded during an entire flux of polar air brought on rapid (Wenatchee Moorpark) suffered winter." It was immediately re- freezing. For six consecutivedays negligible damage. Young Robinia ported that "lossesof strawberries, even the maxima remained below pseudoacaciathat were exceptional- raspberries, blackberries, etc., and the normal minima at Pullman, ly vigorous as a consequenceof small fruits appear to be very Washingtoni The depression was fertilization of the soll were high. Roses, shrubs, and many greater and more enduring than 20 heavily injured, whereas others ornamental trees appear to have years earlier, but the pattern was that had been forced into seasonal been killed. Nurseries suffered strikingly similar, as was the time maturity by drouth and low heavy lossesof plants. Indications of year (Fig. 2, lower half). The fertility survived. A well-estab- are that some orchards may have 1955 .cold wave was the more se- lished tree of the early-maturing been damaged in both divisions of vere, as the depression of maxima Redhaven peach escaped damage the State." This latter proved to below the normal minima was while the later-maturing Rochester be an underestimate. "There was greater, and this phenomenoncon- succumbed. Leaves of many orna- an unusually heavy drop of needles tinued for six consecutivedays. mental trees that were still green from evergreen trees" (native? According to the U.S. Weather were frozen without an absciss exotic?) "after temperatures be- Bureau (11) "new •,inimum tem- layer forming, so that they hung gan to moderate." A preliminary perature records for November on the trees through the winter. estimate of freeze damage to crops were set in many areas during this In fact, a tree of Quercus (coc- was that it "may reach 11 million freeze; the entire State had the cinea?) located at the south edge dollars" (11). A year later the loss coldest weather of record for so of Pullman retained its full com- was reappraised at 66 million early in the season,and it was the plement of dead 1955 leaves dollars. longest period of severe cold ever throughout the summer of 1956, Althou•o'h the cold wave of No- noted in the 66 years of record." along with the new crop. vember 1955 caused no apparent At the writer's home located Native plants at the site west of damage to native plants in eastern about one mile west of Pullmsn. Pullman completely escaped in- Washington and northern Idaho, Washington, 52 speciesor varieties jury. This also applies to plants Taxa native to the seaward side of of woody plants were damaged, in that had been transplanted here the Cascadeswere extensively dam- degrees ranging from slight to on the grasslandfrom'their native aged (2). Injury to native ever- complete killing. Injured patches homes in the relatively cool and green trees there was not uniform. of bark appeared to die at varyin• moist coniferous forests of the It was lighter on the windward times spread over a number of mountains a few miles to the east: sideof the OlympicPeninsula than months, these sometimescompletely Acer glabrum var. douglasii, elsewhere, lighter below an over- girdlin• and thereby killing the Berberis nervosa, Betula p•pyri- story of taller trees: lighter on distal portions of axes or branches. f era, Larix occidentalis,Pachistima northerly rather than on southerly Frequently the girdled stems nut myrsin•tes, Pinus ponderosa, slopes, lighter in the centers of out new leaves at the usual time Pseudotsu6a menziesii (Mirb.) timber tracts rather than along the followino•spring, these.crops of Franco, Sorbus scopulina. How- their margins, lighter wh•re snow leaves dying at varying intervals ever, all three of the "natives" covered seedlingsrather than hav- over the summer. that had been transplanted up- ing been blown off. Tsuga heter- By no means were all the exotics slope from drier climates (Art- ophylla was more severely damaged damaged. Many showed no detri- em,isia rigida, A. tridentata, and than was Thuja p.licata, with mental effects.e.g., pears (Bartlett, Chryso.thamnus n.auseosu• var. Pseudotsuga menziesii least dam- Winter Nellis, Sheldon), sour albicaulis), were included in the aged of the three. The evergreen cherries (Lake Duke), Picea abies, group of plants completely killed. Arbutus menziesii and the decidu- Thu.ia occidentalis, Kolkwitzia Microclimates in the s•all town ous Alnus rubra were extensively am.abilis, and Spgraea vanhoutei. of Pullman were sufficiently dif- killed. The evergreen shrubs Vac- Black raspberries (Cumberland), ferent from those of the surround- cinium ovaturn and Gaultheria oddly enough, gave exceptional ing countryside that damage to shallon were also heavily damaged. yields the following summer. exotics in the town were relatively Severe damage or killing of Strawberries bore normally. light. many exotic trees and shrubs as •No temperature records had been West of the Cascades, "mini- well as a few natives (Alnus rubra, made in Pullman in 1935; this station mum temperatures . . . prior to Comus nuttallii, and Tsuga hetero- is 10 miles from the one at Moscow, this storm . . . had remained above phylla) was also reported at the Idaho, so that the data are closely com- parable. freezing in many of the... areas;" University of Washington Arbore- 584 JOURNAL OF FORESTRY turn, at Seattle (5). It was noted under oceanic climate at the time Washington and Oregon were dam- that young and actively growing of the 1955 freeze. Subsequent aged severely, whereas trees repre- saplings of Cornus nuttallii were tallies of damage showed a distinct senting continental ecotypes were more susceptible than seedlings or tendency toward greater damage damaged lightly or not affected old trees (13). Also, injury to the to thoseplants representing oceanic (3). The latter circumstance is stem "six to eighteen inches above races (4). Also at La Grande, on complementary to the racial test the ground line" was especially the seaward side of the Cascades of Pinus po•,derosawhich is located fatal (13). in Washington, only oceanic eco- in Idaho and provided informa- tion described earlier. It is interesting to compare con- types of Pinus po•clerosa from ditions in northern Idaho and on the west side of the Cascades for this period, since a pair of stations can be selected both of which are IO surrounded by forests containing much Tsuga heterophylla, Thuja plicata, and Pseudotsugamenziesii. 5 Only the Pseud•tsuga has been reco.gnized as taxonomically dis- tinct in the axeas,P. menziesii var. o menziesii to the west of the Cascadesand P.m. var. glauca to -5 the east. The length of the period of below-average temperatures (Fig. 3) and the degreeof depres- -IO sion appear of about equal magni- tudes. Since damage was sustained only by the coastal ecotypes,one -15 might concludethat the ecotypesof the oceanicclimate are genetically Aess adapted to endure deviations -EO from average temperature ranges than are ecotypesof the quasi-conti- nental climate. Stated in another -25 way, the,inland ecotypesare better adapted to their climate than are the coastal races. Since Duffield (2) remarks on variation in dam- age sustained by individuals ex- posed to the same microclimate, it 15 CENTRALIA, WASH. may be postulated that the coastal populationscontain genotypesthat are fairly tolerant of unusual cold I0 conditions, but have not been rigorously purged of the sensitive genotypes as appears to be the case 5 inland. The hypothesis as to the distinct difference in cold tolerance be- 0 tween oceanicand quasi-continental ecotypes, suggested by the cir- cumstances described above, is -5 strengthened by two further ob- servations. In a nursery located -I0 on the campus of the University of British Columbia at Vancouver, iiIII B.C., about a hundred feet above -15' sea level and a few hundred yards from the sea, 2-year-old seedlings FIo. 3.--Comparison of the character of one cold period, -20, 1955, as of Pseudotsugame•ziesii represent- recorded 50 miles from the ocean at Centralia, Washington, and 300 miles from the ocean at Pullman, Washington. Both areas are in forests where Tsuga hetero- ing both oceanic and continental phylla, Thuja plicata, and Pseudotsuga menziesii are comon trees, but these trees ecotypeshad grown for two years were damaged only near the coast. 1957 585

Discussion plete lack of any factual support pearsto be the sameon both sides of the Cascades,it may be con- A conclusion that the shoots of for areas regularly subjected to cluded that the coastal ecotypesof oceanic ecotypes are damaged by freezing weather in winter (1). Severe as they were, the botanical shrubs and trees are less well sudden drops in temperature in adapted to their climate than are late autumn or early winter, where- consequencesof the three extreme freezes reported above show that the inland ecotypes. This conclu- as ecotypesfrom quasi-continental sion is borne out by divergent be- climates are little if at all dam- for the region and time span con- cerned, temperature extremes havior of inland and coastal races aged, seemswell supported by the would have to be much more vio- planted together in both climatic observations reported above. It lent to cause enough disruption of regions. It would appear that on rests upon the divergent responses account of their hardiness, the use of unintentional but nevertheless life cycles to becomea key factor determining plant ranges. Heavy of inland ecotypes might be less fully satisfactory reciprocal trans- damage or even death of exotics is risky in coastal plantations produc- plants of Pinus ponderosa races not valid evidence for the hypoth- ing Christmas trees. Despite the grown in both climatic types, upon esis, since exotics are planted well conspicuousdamage and great eco- the divergent responsesof diverse nomic loss resulting from these races of Pseudotsuga menziesii beyond their natural ranges. Critical support for the hypothesis three cold waves, there is no evid- grown in oceanicclimate, and upon must consist of depopulation of at ence in the 67 years of weather the differences in damage sustained least a sector of at least a thin records in this area that low tem- by native vegetation in two regions peripheral belt about a plant's perature extremes have any influ- where the .degree of severity of ence in determining the ranges of freezing appears equivalent. range, and although many native plants are at the margins of their native plants. One practical application of this ranges in Washington and north- conclusion is suggested.There is a Literature Cited growing industry in the vicinity ern Idaho, none of these is known to have suffered any damage to of large metropolitan districts near 1. DAUBEN'MIRE, R. 1956. Climate as a their aerial parts that cannot be determinant of vegetation distribu- the coastbased upon growing small completely repaired by one or two tion in eastern Washington and trees of Pseudotsugamenziesii that northern Idaho. Eeol. Mono. 26:131- near-normal seasons. are harvested in a short rotation 154. 2. DUPPIELD, J. W. 1956. Damage to and sold for decorations at the Summary western Washington forests from Christmas season. Since only sym- November 1955 cold wave. Pacific Abrupt invasions of abnormally Northwest Forest & Range Expt. metrical and healthy trees are cold air masses in late autumn or Sta. Res. Note 129. salable, and sudden drops in tem- early winter have been recorded in 3. GESSEL, S. P. 1957. Based on un- perature may be expected to cause published data which were gen- Washington and northern Idaho in erously furnished through corres- severe economic damage to the 1924, 1935, and 1955. Exotic plants pondence. plantations at intervals of perhaps were damaged and sometimescom- 4. HADdocK, P. G. 1957. Based on un- only a few rotations, the risk in- published data which were generous- pletely killed during each of these ly furnished through correspondence. volved in using coastal ecotypes cold waves. In one garden at Pull- 5. I•ULLI(]AN, B. O. 1956. Trees killed might be avoided through the use man, Washington, all (eight) by cold weather, -18, of inland ecotypes instead. The 1955, at University of Washington woody plants transplanted here Arboretum, Seattle. Univ. of Wash. leasability of this practice would, from wetter climates immediately Arboretum. Miracog. of course, hinge upon finding at to the east survived without injury, 6. U.S. WEATHER BUREAU. 1924. Cli- matological data. 27 (Idaho Sec., least one inland ecotype with whereas all (three) woody plants No. 12) :52. growth rate, susceptibility to dis- that had been transplanted here 7. 1924. Climatological ease, or other characteristics that from drier climates immediately to data.28 (•ash. Sec.,No. 12).51. 8. 1935. Climatological did not nullify the advantage of the west were killed completely. data.38 (•dahoSea., No. 10):46; superior cold tolerance. Native plants in the quasi-contin- 38 (Idaho Sec., No. 11):50. 9. 1935. Climatological The freeze phenomena also have ental climate of eastern Washing- data.39 (•Vash.Sec., No. 11):81. a bearing upon ecologicplant geo- ton and northern Idaho appear not 10. 1955. Climatological graphy. An hypothesis has been to have been damaged, but in the data.41 (•ash. Sec.,No. 11) 11. 1956. Climatological advanced that the limits of plant oceanic climate to the west of the data.41 (•Vash.Sec., No. 13):206. ranges may be set by .climatic ex- Cascades there was extensive dam- 12. WE•DMA•, R. H. 1939. Evidences of tremes, but this has been recently age to natives in 1955 and possibly racial influence in a 25-year old test also in 1935. Since the relative ab- of ponderosa pine. Jour. Agrie. Res. reviewed in detail and challenged 59: 855-888. in part by pointing out the corn- normality of the cold waves ap- 13. W•r, J. A. 1957. Correspondence.