<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>11</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/hess-11-1013-2007</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/11/1013/2007/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/11/1013/2007/hess-11-1013-2007.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/11/1013/2007/hess-11-1013-2007.pdf</fulltext_pdf>
	<start_page>1013</start_page>
	<end_page>1033</end_page>
	<publication_date>2007-03-27</publication_date>
	<article_title content_type="html">Biotic pump of atmospheric moisture as driver of the hydrological cycle on land</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. M. Makarieva</name>
			<email>elba@infopro.spb.su</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. G. Gorshkov</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Petersburg Nuclear Physics Institute, Gatchina, St. Petersburg, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper the basic geophysical and ecological principles are jointly
analyzed that allow the landmasses of Earth to remain moistened
sufficiently for terrestrial life to be possible. 1. Under gravity, land
inevitably loses water to the ocean. To keep land moistened, the
gravitational water runoff must be continuously compensated by the
atmospheric ocean-to-land moisture transport. Using data for five
terrestrial transects of the International Geosphere Biosphere Program we
show that the mean distance to which air fluxes
can transport moisture over non-forested areas, does not exceed several
hundred kilometers; precipitation decreases exponentially with distance
from the ocean. 2. In contrast, precipitation over extensive natural
forests does not depend on the distance from the ocean along several
thousand kilometers, as illustrated for the Amazon and Yenisey river
basins and Equatorial Africa. This points to the existence of an active
biotic pump transporting atmospheric moisture inland from the ocean. 3. Physical
principles of the biotic moisture pump are investigated based on
the previously unstudied properties of atmospheric water vapor, which can
be either in or out of aerostatic equilibrium depending on the lapse
rate of air temperature. A novel physical principle is formulated
according to which the low-level air moves from areas with weak
evaporation to areas with more intensive evaporation. Due to the high
leaf area index, natural forests maintain high evaporation fluxes,
which support the ascending air motion over the forest and &quot;suck in&quot;
moist air from the ocean, which is the essence of the biotic pump of
atmospheric moisture. In the result, the gravitational runoff water
losses from the optimally moistened forest soil can be fully compensated
by the biotically enhanced precipitation at any distance from the ocean.
4. It is discussed how a continent-scale biotic water pump mechanism
could be produced by natural selection acting on individual trees. 5. Replacement
of the natural forest cover by a low leaf index vegetation
leads to an up to tenfold reduction in the mean continental precipitation
   and runoff, in contrast to the previously available estimates made
without accounting for the biotic moisture pump. The analyzed body of
evidence testifies that the long-term stability of an intense terrestrial
water cycle is unachievable without the recovery of natural,
self-sustaining forests on continent-wide areas.</abstract>
	<references>
		<reference numeration="1" content_type="text">Acevedo, O. C., Moraes, O. L. L.,           da Silva, R., Fitzjarrald, D. R., Sakai, R. K., Staebler, R. M., and Czikowsky, M. J.: Inferring nocturnal surface fluxes from vertical profiles of scalars in an Amazon pasture, Global Change Biology, 10, 886&amp;ndash;894, 2004. </reference>
		<reference numeration="2" content_type="text"> Adler, R. F., Huffman, G. J., Bolvin, D. T., Curtis, S., and Nelkin, E. J.: Tropical rainfall distributions determined using TRMM combined with other satellite and rain gauge, J. Appl. Meteorol., 39, 2007&amp;ndash;2023, 2001. </reference>
		<reference numeration="3" content_type="text"> Arora, V.: Comment on &quot;Optimized stomatal conductance of vegetated land surfaces and its effects on simulated productivity and climate&quot; edited by: Kleidon, A., Geophys. Res. Lett., 32, L08708, doi:10.1029/2004GL022110, 2005. </reference>
		<reference numeration="4" content_type="text"> Austin, A. T. and Sala, O. E.: Carbon and nitrogen dynamics across a natural precipitation gradient in Patagonia, Argentina, J. Vegetation Sci., 13, 351&amp;ndash;360, 2002. </reference>
		<reference numeration="5" content_type="text"> Austin, A. T. and Vitousek, P. M.: Precipitation, decomposition and litter decomposability of Metrosideros polymorpha in native forests on Hawaii, J. Ecology, 88, 129&amp;ndash;138, 2000. </reference>
		<reference numeration="6" content_type="text"> Baerlocher, F.: The Gaia hypothesis: A fruitful fallacy?, Experientia, 46, 232&amp;ndash;238, 1990. </reference>
		<reference numeration="7" content_type="text"> Barrett, J. E., McCulley, R. L., Lane, D. R., Burke, I. C., and Lauenroth, W. K.: Influence of climate variability on plant production and N-mineralization in Central US grasslands, J. Vegetation Sci., 13, 383&amp;ndash;394, 2002. </reference>
		<reference numeration="8" content_type="text"> Bond, B. J. and Kavanagh, K. L.: Stomatal behavior of four woody species in relation to leaf-specific hydraulic conductance and threshold water potential, Tree Physiology, 19, 503&amp;ndash;510, 1999. </reference>
		<reference numeration="9" content_type="text">Bowman, D. M. J. S.: The Australian summer monsoon: a biogeographic perspective, Australian Geographic Studies, 40, 261&amp;ndash;277, 2002. </reference>
		<reference numeration="10" content_type="text">Breshears, D. D., Nyhan, J. W., Heil, C. E., and Wilcox, B. P.: Effects of woody plants on microclimate in a semiarid woodland: soil temperature and evaporation in canopy and intercanopy patches, Int. J. Plant Sci., 159, 1010&amp;ndash;1017, 1998. </reference>
		<reference numeration="11" content_type="text"> Bryant, D., Nielsen, D., and Tangley, L.: The last frontier forests: ecosystems and economies on the edge, World Resources Institute, Washington, 1997. </reference>
		<reference numeration="12" content_type="text"> Cabido, M., Gonzalez, C., Acosta, A., and Diaz, S.: Vegetation changes along a precipitation gradient in central Argentina, Vegetatio, 109, 5&amp;ndash;14, 1993. </reference>
		<reference numeration="13" content_type="text"> Canadell, J G., Steffen, W L., and White, P S.: IGBP/GCTE terrestrial transects: Dynamics of terrestrial ecosystems under environmental change &amp;ndash; Introduction, J. Vegetation Sci., 13, 297&amp;ndash;300, 2002. </reference>
		<reference numeration="14" content_type="text">Cochrane, M. A., Alencar, A., Schulze, M. D., Souza, C. M., Nepstad, D. C., Lefebvre, P., and Davidson, E. A.: Positive feedbacks in the fire dynamic of closed canopy tropical forests, Science, 284, 1832&amp;ndash;1835, 1999.  </reference>
		<reference numeration="15" content_type="text"> Coley, P. D. and Barone, J. A.: Herbivory and plant defenses in tropical forests, Annual Review of Ecology and Systematics, 27, 305&amp;ndash;335, 1996. </reference>
		<reference numeration="16" content_type="text"> Cook, G. D. and Heerdegen, R. G.: Spatial variation in the duration of the rainy season in monsoonal Australia, Int. J. Climatology, 21, 1723&amp;ndash;1732, 2001. </reference>
		<reference numeration="17" content_type="text"> da Rocha, H. R., Goulden, M. L., Miller, S. D., Menton, M. C., Pinto, L. D. V. O., de Freitas, H. C., and Silva Figueira, A. M. E.: Seasonality of water and heat fluxes over a tropical forest in eastern Amazonia, Ecological Appl., 14(Suppl), S22&amp;ndash;S32, 2004. </reference>
		<reference numeration="18" content_type="text"> Dai, A. and Trenberth, K E.: Estimates of freshwater discharge from continents: latitudinal and seasonal variations, J. Hydrometeorol., 3, 660&amp;ndash;687, 2002. </reference>
		<reference numeration="19" content_type="text"> Doolittle, W. F.: Is nature really Motherly?, CoEvolution Quaterly, 29, 58&amp;ndash;63, 1981. </reference>
		<reference numeration="20" content_type="text"> Fang, M. and Tung, K. K.: Time-dependent nonlinear Hadley circulation, J. Atmos. Sci., 56, 1797&amp;ndash;1807, 1999. </reference>
		<reference numeration="21" content_type="text"> Folkins, I.: Convective damping of buoyancy anomalies and its effect on lapse rates in the tropical lower troposphere, Atmos. Chem. Phys., 6, 1&amp;ndash;12, 2006. </reference>
		<reference numeration="22" content_type="text"> Goody, R. M. and Yung, Y. L.: Atmospheric radiation, theoretical basis, 2nd edn, Oxford Univ. Press, New York, 1989. </reference>
		<reference numeration="23" content_type="text"> Gorshkov, V. G.: Ecology of man, Leningrad Polytechnical Institute, Leningrad, 1984. </reference>
		<reference numeration="24" content_type="text"> Gorshkov, V. G.: Physical and biological bases of life stability, Springer, Berlin, 1995. </reference>
		<reference numeration="25" content_type="text"> Gorshkov, V. G. and Makarieva, A. M.: On the possibility of physical self-organization of biological and ecological systems, Doklady Biological Sci., 378, 258&amp;ndash;261, 2001. </reference>
		<reference numeration="26" content_type="text"> Gorshkov, V. G., Gorshkov, V. V., and Makarieva, A. M.: Biotic regulation of the environment: Key issue of global change, Springer, London, 2000. </reference>
		<reference numeration="27" content_type="text">Gorshkov, V. G., Makarieva, A. M., and Gorshkov, V. V.: Revising the fundamentals of ecological knowledge: The biota-environment interaction, Ecol. Complexity, 1, 17&amp;ndash;36, 2004. </reference>
		<reference numeration="28" content_type="text"> Goulden, M. L., Daube, B. C., Fan, S.-M., Sutton, D. J., Bazzaz, A., Munger, J. W., and Wofsy, S. C.: Physiological response of a black spruce forest to weather, J. Geophys. Res., 102D, 28 987&amp;ndash;28 996, 1997. </reference>
		<reference numeration="29" content_type="text"> Goulden, M. L., Miller, S. D., da Rocha, H. R., Menton, M. C., de Freitas, H. C., Silva Figueira, A. M. E., and de Sousa, C. A. D.: Diel and seasonal patterns of tropical forest \chemCO_2 exchange, Ecol. Appl., 14(Suppl), S42&amp;ndash;S54, 2004. </reference>
		<reference numeration="30" content_type="text">Gustavson, M. R.: Limits to the wind power  utilization, Sci., 204, 13&amp;ndash;17, 1979. </reference>
		<reference numeration="31" content_type="text"> Hodnett, M. G., Oyama, M. D., Tomasella, J., and Marques Filho, A. de O.: Comparisons of long-term soil water storage behaviour under pasture and forest in three areas of Amazonia, in: Amazonian deforestation and climate, edited by: Gash, J. H. C., Nobre, C. A., Roberts, J. M., and Victoria, R. L., 57&amp;ndash;77, John Wiley &amp; Sons, Chichester, 1996. </reference>
		<reference numeration="32" content_type="text"> Hutley, L. B., O&apos;Grady, A. P., and Eamus, D.: Monsoonal influences on evapotranspiration of savanna vegetation of northern Australia, Oecologia, 126, 434&amp;ndash;443, 2001. </reference>
		<reference numeration="33" content_type="text"> Karlsson, I. M.: Nocturnal air temperature variations between forest and open areas, J. Appl. Meteorol., 39, 851&amp;ndash;862, 2000. </reference>
		<reference numeration="34" content_type="text"> Kleidon, A.: Optimized stomatal conductance of vegetated land surfaces and its effects on simulated productivity and climate, Geophys. Res. Lett., 31, L21203, doi:10.1029/2004GL020769, 2004. </reference>
		<reference numeration="35" content_type="text"> Kleidon, A.: Reply to comment by V. Arora on &quot;Optimized stomatal conductance of vegetated land surfaces and its effects on simulated productivity and climate&quot;, Geophys. Res. Lett., 32, L08709, doi:10.1029/2005GL022355, 2005. </reference>
		<reference numeration="36" content_type="text">Kruijt, B., Malhi, Y., Lloyd, J., Nobre, A. D., Miranda, A. C., Pereira, M. G. P.,           Culf, A., and Grace, J.: Turbulence statistics above and within two Amazon rain forest canopies, Boundary-Layer Meteorol., 94, 297&amp;ndash;331, 2000.  </reference>
		<reference numeration="37" content_type="text"> Kurc, S. A. and Small, E.E.: Dynamics of evapotranspiration in semiarid grassland and shrubland ecosystems during the summer monsoon season, central New Mexico, Water Resour. Res., 40, W09305, doi:10.1029/2004WR003068, 2004. </reference>
		<reference numeration="38" content_type="text"> Lal, R.: Soil erosion and land degradation: the global risks, in: Advances in soil science, 11, Soil degradation, edited by: Lal, R. and Stewart, B. A., 129&amp;ndash;172, Springer, New York, 1990. </reference>
		<reference numeration="39" content_type="text"> Landau, L. D., Akhiezer, A. I., and Lifshitz, E. M.: General Physics., Mechanics and Molecular Physics, Nauka, Moscow, 1965. </reference>
		<reference numeration="40" content_type="text"> Landau, L. D. and Lifshitz, E. M.: Course of Theoretical Physics, 6, Fluid Mechanics, 2nd ed., Butterworth-Heinemann, Oxford, 1987. </reference>
		<reference numeration="41" content_type="text"> Lorenz, E. N.: The nature and theory of the general circulation of the atmosphere, World Meteorological Organization, Geneva, 1967. </reference>
		<reference numeration="42" content_type="text"> L&apos;vovitch, M. I.: World water resources and their future, American Geological Union, Washington, 1979. </reference>
		<reference numeration="43" content_type="text">Mahrt, L., Lee, X., Black, A., Neumann, H., and Staebler, R. M.: Nocturnal mixing in a forest subcanopy, Agric. Forest Meteorol., 101, 67&amp;ndash;78, 2000. </reference>
		<reference numeration="44" content_type="text">Makarieva, A. M.,  Gorshkov, V. G., and Li, B.-L.: Biochemical universality of living matter and its metabolic implications, Functional Ecol., 19, 547&amp;ndash;557, 2005a. </reference>
		<reference numeration="45" content_type="text">Makarieva, A. M.,  Gorshkov, V. G., and Li, B.-L.: Revising the distributive networks models of West, Brown and Enquist (1997) and Banavar, Maritan and Rinaldo (1999): Metabolic inequity of living tissues provides clues for the observed allometric scaling rules, J. Theor. Biol., 237, 291&amp;ndash;301, 2005b. </reference>
		<reference numeration="46" content_type="text">Makarieva, A. M., Gorshkov, V. G., and Li, B.-L.: Energetics of the smallest: Do bacteria breathe at the same rate as whales?, Proceedings of the Royal Society of London B, 272, 2219&amp;ndash;2224, 2005c. </reference>
		<reference numeration="47" content_type="text"> Marengo, J. A.: Interdecadal variability and trends of rainfall across the Amazon basin, Theor. Appl. Climatology, 78, 79&amp;ndash;96, 2004. </reference>
		<reference numeration="48" content_type="text"> McEwan, M. J. and Phillips L. F.: Chemistry of the atmosphere, Edward Arnold, London, 1975.  </reference>
		<reference numeration="49" content_type="text"> McGuffie, K. and Henderson-Sellers, A.: Forty years of numerical climate modelling, Int. J. Climatology, 21, 1067&amp;ndash;1109, 2001. </reference>
		<reference numeration="50" content_type="text"> McGuire, A. D., Prentice, I. C., Ramankutty, N., Reichenau, T., Schloss, A., Tian, H., Williams, L. J., and Wittenberg, U.: Carbon balance of the terrestrial biosphere in the twentieth century: Analyses of \chemCO_2, climate and land-use effects with four process-based ecosystem models, Global Biogeochem. Cycles, 15, 183&amp;ndash;206, 2001. </reference>
		<reference numeration="51" content_type="text"> Miller, J. M., Williams, R. J., and Farquhar, G. D.: Carbon isotope discrimination by a sequence of Eucalyptus species along a subcontinental rainfall gradient in Australia, Funct. Ecol., 15, 222&amp;ndash;232, 2001. </reference>
		<reference numeration="52" content_type="text">Nepstad, D., Lefebvre, P., da Silva, U. L., Tomasella, J., Schlesinger, P., Solorzano, L., Ray, P. M. D., and Benito, J. G.: Amazon drought and its implications for forest flammability and tree growth: a basin-wide analysis, Global Change Biol., 10, 704&amp;ndash;717, 2004. </reference>
		<reference numeration="53" content_type="text">Nesbitt, S. W. and Zipser, E. J.: The diurnal cycle of rainfall and convective intensity according to three years of TRMM measurements, J. Climate, 16, 1456&amp;ndash;1475, 2003. </reference>
		<reference numeration="54" content_type="text"> Ni, J. and Zhang, X. S.: Climate variability, ecological gradient and the Northeast China Transect (NECT), J. Arid Environments, 46, 313&amp;ndash;325, 2000. </reference>
		<reference numeration="55" content_type="text"> Nicholson, S. E.: The nature of rainfall variability over Africa on time scales of decades to millenia, Global Planet. Change, 26, 137&amp;ndash;158, 2000. </reference>
		<reference numeration="56" content_type="text"> Oyama, M. D. and Nobre, C. A.: Climatic consequences of a large-scale desertification in Northeast Brazil: A GCM simulation study, J. Climate, 17, 3203&amp;ndash;3213, 2004. </reference>
		<reference numeration="57" content_type="text">Randel, D. L., Haar, T. H. V.,                  Ringerud, M. A., Stephens, G. L., Greenwald, T. J., and Comb, C. L.: New global water vapor dataset, Bulletin of the American Meteorol. Society, 77, 1233&amp;ndash;1254, 1996.  </reference>
		<reference numeration="58" content_type="text"> Savenije, H H G.: New definitions for moisture recycling and the relationship with land-use change in the Sahel, J. Hydrology, 167, 57&amp;ndash;78, 1995. </reference>
		<reference numeration="59" content_type="text"> Savenije, H H G.: Does moisture feedback affect rainfall significantly?, Physics Chem. Earth, 20, 507&amp;ndash;513, 1996a. </reference>
		<reference numeration="60" content_type="text"> Savenije, H H G.: The runoff coefficient as the key to moisture recycling, Journal of Hydrology, 176, 219&amp;ndash;225, 1996b. </reference>
		<reference numeration="61" content_type="text"> Savenije, H. H. G.: The importance of interception and why we should delete the term evapotranspiration from our vocabulary, Hydrol. Processes, 18, 1507&amp;ndash;1511, 2004.  </reference>
		<reference numeration="62" content_type="text"> Shver, C. A.: Atmospheric precipitation on the territory of the USSR, Meteoizdat, Leningrad, 1976. </reference>
		<reference numeration="63" content_type="text">Shuttleworth, W. J.: Micrometeorology of temperate and tropical forest, Philosophical Transactions of the Royal Society of London B, 324, 207&amp;ndash;228, 1989. </reference>
		<reference numeration="64" content_type="text">Shuttleworth, W. J., Gash, J. H. C., Lloyd, C. R., Moore, C. J., Roberts, J., Marques-Filho, A. O., Fisch, G., Filho, V. P. S., Ribeiro, M. N. G.,              Molion, L. C. B., Sa, L. D. A., Nobre, J. C. A., Cabral, O. M. R., Patel, S. R., and Carvalho, J. M.: Daily variations of temperature and humidity within and above Amazonian forest, Weather, 40, 102&amp;ndash;108, 1985.  </reference>
		<reference numeration="65" content_type="text"> Smith, S. B.: Comments on &quot;An interesting mesoscale storm-environment interaction observed just prior to changes in severe storm behavior&quot;, Weather and Forecasting, 12, 368&amp;ndash;372, 1997. </reference>
		<reference numeration="66" content_type="text">Szarzynski, J. and Anhuf, D.: Micrometeorological conditions and canopy energy exchanges of a neotropical rain forest (Surumoni-Crane Project, Venezuela), Plant Ecol., 153, 231&amp;ndash;239, 2001. </reference>
		<reference numeration="67" content_type="text"> Tchebakova, N. M., Kolle ,O., Zolotoukhine, D., Arneth, A., Styles, J. M., Vygodskaya, N. N., Schulze, E.-D., Shibistova, O., and Lloyd, J.: Inter-annual and seasonal variations of energy and water vapor fluxes above a Pinus sylvestris forest in the Siberian middle taiga, Tellus B, 54, 537&amp;ndash;551, 2002. </reference>
		<reference numeration="68" content_type="text">Tutin, C. E. G., White, L. J. T., and Mackanga-Missandzou, A.: The use by rain forest mammals of natural forest fragments in an equatorial African Savanna, Conservation Biol., 11, 1190&amp;ndash;1203, 1997. </reference>
		<reference numeration="69" content_type="text">Van de Koppel, J. and Prins, H. H. T.: The importance of herbivore interactions for the dynamics of African savanna woodlands: an hypothesis, J. Tropical Ecol., 14, 565&amp;ndash;576, 1998. </reference>
		<reference numeration="70" content_type="text"> Weaver, C. P. and Ramanathan, V.: Deductions from a simple climate model: Factors governing surface temperature and atmospheric thermal structure, J. Geophys. Res., 100D, 11 585&amp;ndash;11 591, 1995. </reference>
		<reference numeration="71" content_type="text">Webber, S. R. and Wilmott, C. J.: South American Precipitation: 1960&amp;ndash;1990 gridded monthly time series (version 1.02), Center for Climatic Research, Department of Geography, University of Delaware, Newark, Delaware, 1998. </reference>
		<reference numeration="72" content_type="text"> Werth, D. and Avissar, R.: The regional evapotranspiration of the Amazon, J. Hydrometeorol., 5, 100&amp;ndash;109, 2004. </reference>
		<reference numeration="73" content_type="text"> Zhou, J. and Lau, K.-M.: Does a monsoon climate exist over South America?, J. Climate, 11, 1020&amp;ndash;1040, 1998. </reference>
	</references>
</article>

