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Holdridge life zones

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480: 133: 36: 519: 558:: unlike the more developed areas facing the same shift, it is suggested they would struggle to adapt due to limited social resilience, and so crop and livestock in those places would leave what the authors have defined as a "safe climatic space". On a global scale, that results in 31% of crop and 34% of livestock production being outside of the safe climatic space. 237:
Biotemperature is based on the growing season length and temperature. It is measured as the mean of all annual temperatures, with all temperatures below freezing and above 30 °C adjusted to 0 °C, as most plants are dormant at these temperatures. Holdridge's system uses biotemperature first,
515:, as shifts in life zones happening in a matter of decades inherently result in unstable weather conditions compared to what that area had experienced throughout human history. Developed regions may be able to adjust to that, but those with fewer resources are less likely to do so. 725: 483:
On this map, a shift of 1 indicates that at the end of the century, the region had fully moved into a completely different Holdridge zone type from where it had been historically. The extent of the shifts will be dependent on the severity of the
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zones too, but is less applicable to cold oceanic or cold arid climates where moisture becomes the predominant factor. The system has found a major use in assessing the potential changes in natural vegetation patterns due to
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Areas of the globe where agriculture would become more difficult perhaps to the point of leaving the conditions historically suitable for it, under low-emission and high-emission scenarios, by 2100.
265:(ET) is the raw sum of evaporation and plant transpiration from the Earth's land surface to atmosphere. Evapotranspiration can never be greater than PET. The ratio, Precipitation/PET, is the 136:
Holdridge life zone classification scheme. Although conceived as three-dimensional by its originator, it is usually shown as a two-dimensional array of hexagons in a triangular frame.
297: 934: 284:. In the warmer regions, there are deserts with maximum PET but low rainfall that make the soil even drier, and rain forests with low PET and maximum rainfall causing 148:
in 1947, and updated in 1967. It is a relatively simple system based on few empirical data, giving objective criteria. A basic assumption of the system is that both
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While it was first designed for tropical and subtropical areas, the system now applies globally. The system has been shown to fit not just
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Harris SA (1973). "Comments on the Application of the Holdridge System for Classification of World Life Zones as Applied to Costa Rica".
929: 505: 470: 119: 100: 496:, with more severe change resulting in more remarkable shifts in a geologically rapid time span, leaving less time for humans and 599: 589: 72: 57: 79: 504:
fail to adapt to these changes, they would ultimately go extinct: the scale of future change also determines the extent of
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Many areas of the globe are expected to see substantial changes in their Holdridge life zone type as the result of
242:'s life zones, and does not primarily consider elevation directly. The system is considered more appropriate for 68: 670: 527: 416: 485: 185: 46: 411: 574: 447: 276:
The coldest regions have not much evapotranspiration nor precipitation as there is not enough heat to
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is a global bioclimatic scheme for the classification of land areas. It was first published by
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In contrast, under the low-emissions SSP1-2.6 (a scenario compatible with the less ambitious
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output would experience very rapid shift in its Holdridge Life Zones. This includes most of
325: 173: 153: 145: 562: 555: 257:(PET) is the amount of water that would be evaporated and transpired if there were enough 873: 705: 565:
goals, 5% and 8% of crop and livestock production would leave that safe climatic space.
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Kummu, Matti; Heino, Matias; Taka, Maija; Varis, Olli; Viviroli, Daniel (21 May 2021).
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For humanity, this phenomenon has particularly important implications for
671:"Possible Changes in Natural Vegetation Patterns Due to a Global Warming" 526:
Some research suggests that under the scenario of continually increasing
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Global bioclimatic scheme for the classification of land areas
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Scientific relationship between the 3 axes and 3 indicators
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All the classes defined within the system, as used by the
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available. Higher temperatures result in higher PET.
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Further indicators incorporated into the system are:
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International Institute for Applied Systems Analysis
817:Parry, M. L.; Carter, T. R.; Konijn, N. T. (1988), 60:. Unsourced material may be challenged and removed. 8: 851: 849: 847: 845: 673:. National Geophysical Data Center (NOAA). 288:systems to drain excess water into oceans. 238:rather than the temperate latitude bias of 935:Climate and weather classification systems 889: 156:can be mapped once the climate is known. 120:Learn how and when to remove this message 475:Effects of climate change on agriculture 611: 802:: CS1 maint: archived copy as title ( 795: 7: 58:adding citations to reliable sources 820:The effects on Holdridge Life Zones 506:extinction risk from climate change 471:Effects of climate change on biomes 269:(AI), with an AI<0.2 indicating 208:ratio (PET) to mean total annual 25: 731:from the original on 27 May 2015 714:10.1046/j.1365-2699.1999.00329.x 677:from the original on 2009-10-16. 600:Trewartha climate classification 273:, and AI<0.5 indicating dry. 34: 619:US EPA, OA (January 29, 2013). 45:needs additional citations for 751:"potential_evapotranspiration" 1: 590:Köppen climate classification 882:10.1016/j.oneear.2021.04.017 255:Potential evapotranspiration 206:potential evapotranspiration 184:The three major axes of the 779:agron-www.agron.iastate.edu 390:Warm temperate moist forest 381:Warm temperate desert scrub 369:Cool temperate moist forest 142:Holdridge life zones system 951: 930:Geographic classifications 644:Arctic and Alpine Research 468: 408:Subtropical thorn woodland 396:Warm temperate rain forest 384:Warm temperate thorn scrub 375:Cool temperate rain forest 202:(mean annual, logarithmic) 393:Warm temperate wet forest 387:Warm temperate dry forest 372:Cool temperate wet forest 528:greenhouse gas emissions 439:Tropical very dry forest 417:Subtropical moist forest 405:Subtropical desert scrub 186:barycentric subdivisions 694:Journal of Biogeography 486:climate change scenario 436:Tropical thorn woodland 424:Subtropical rain forest 246:than Merriam's system. 755:esdac.jrc.ec.europa.eu 550:, as well as parts of 523: 489: 421:Subtropical wet forest 412:Subtropical dry forest 168:vegetation zones, but 137: 69:"Holdridge life zones" 669:Leemans, Rik (1990). 575:Andrew Delmar Hopkins 521: 482: 448:Tropical moist forest 433:Tropical desert scrub 378:Warm temperate desert 316:Subpolar moist tundra 195:(annual, logarithmic) 135: 925:Sustainable building 920:Biogeographic realms 688:Lugo, A. E. (1999). 458:Tropical rain forest 322:Subpolar rain tundra 54:improve this article 874:2021OEart...4..720K 706:1999JBiog..26.1025L 453:Tropical wet forest 443:Tropical dry forest 319:Subpolar wet tundra 244:tropical vegetation 227:latitudinal regions 18:Holdridge life zone 631:on April 28, 2013. 552:sub-Saharan Africa 524: 490: 348:Boreal rain forest 280:much water, hence 263:Evapotranspiration 138: 830:978-94-009-2965-4 345:Boreal wet forest 232:altitudinal belts 154:climax vegetation 130: 129: 122: 104: 16:(Redirected from 942: 904: 903: 893: 853: 840: 839: 838: 837: 814: 808: 807: 801: 793: 791: 790: 781:. Archived from 771: 765: 764: 762: 761: 747: 741: 740: 738: 736: 730: 700:(5): 1025–1038. 685: 679: 678: 666: 660: 659: 650:(3): A187–A191. 639: 633: 632: 627:. Archived from 616: 146:Leslie Holdridge 125: 118: 114: 111: 105: 103: 62: 38: 30: 21: 950: 949: 945: 944: 943: 941: 940: 939: 910: 909: 908: 907: 855: 854: 843: 835: 833: 831: 816: 815: 811: 794: 788: 786: 775:"Archived copy" 773: 772: 768: 759: 757: 749: 748: 744: 734: 732: 728: 687: 686: 682: 668: 667: 663: 641: 640: 636: 618: 617: 613: 608: 571: 563:Paris Agreement 556:Central America 477: 467: 462: 363:Cool temperate 357:Cool temperate 294: 252: 162: 126: 115: 109: 106: 63: 61: 51: 39: 28: 23: 22: 15: 12: 11: 5: 948: 946: 938: 937: 932: 927: 922: 912: 911: 906: 905: 868:(5): 720–729. 841: 829: 809: 766: 742: 680: 661: 634: 610: 609: 607: 604: 603: 602: 597: 592: 587: 582: 577: 570: 567: 500:to adjust. If 494:climate change 466: 465:Climate change 463: 461: 460: 455: 450: 445: 440: 437: 434: 431: 425: 422: 419: 414: 409: 406: 403: 397: 394: 391: 388: 385: 382: 379: 376: 373: 370: 367: 361: 355: 352:Cool temperate 349: 346: 343: 337: 331: 323: 320: 317: 314: 308: 302: 300:(IIASA), are: 293: 290: 271:arid/hyperarid 251: 248: 235: 234: 229: 224: 214: 213: 203: 196: 179:global warming 161: 158: 128: 127: 42: 40: 33: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 947: 936: 933: 931: 928: 926: 923: 921: 918: 917: 915: 901: 897: 892: 887: 883: 879: 875: 871: 867: 863: 859: 852: 850: 848: 846: 842: 832: 826: 822: 821: 813: 810: 805: 799: 785:on 2020-01-28 784: 780: 776: 770: 767: 756: 752: 746: 743: 727: 723: 719: 715: 711: 707: 703: 699: 695: 691: 684: 681: 676: 672: 665: 662: 657: 653: 649: 645: 638: 635: 630: 626: 622: 615: 612: 605: 601: 598: 596: 593: 591: 588: 586: 583: 581: 578: 576: 573: 572: 568: 566: 564: 559: 557: 553: 549: 545: 541: 537: 533: 529: 520: 516: 514: 509: 507: 503: 499: 495: 487: 481: 476: 472: 464: 459: 456: 454: 451: 449: 446: 444: 441: 438: 435: 432: 429: 426: 423: 420: 418: 415: 413: 410: 407: 404: 401: 398: 395: 392: 389: 386: 383: 380: 377: 374: 371: 368: 366: 362: 360: 356: 353: 350: 347: 344: 342: 339:Boreal moist 338: 336: 332: 330: 327: 324: 321: 318: 315: 313: 310:Subpolar dry 309: 307: 304: 303: 301: 299: 291: 289: 287: 283: 282:polar deserts 279: 274: 272: 268: 267:aridity index 264: 260: 256: 249: 247: 245: 241: 233: 230: 228: 225: 222: 219: 218: 217: 211: 210:precipitation 207: 204: 201: 197: 194: 193:precipitation 191: 190: 189: 187: 182: 180: 175: 171: 170:Mediterranean 167: 159: 157: 155: 151: 147: 143: 134: 124: 121: 113: 110:December 2021 102: 99: 95: 92: 88: 85: 81: 78: 74: 71: –  70: 66: 65:Find sources: 59: 55: 49: 48: 43:This article 41: 37: 32: 31: 19: 865: 861: 834:, retrieved 819: 812: 787:. 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Holdridge life zone

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Leslie Holdridge
soil
climax vegetation
tropical
Mediterranean
boreal
global warming
barycentric subdivisions
precipitation
temperature
potential evapotranspiration
precipitation
humidity
latitudinal regions
altitudinal belts
Merriam
tropical vegetation

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