Èçìåíåíèÿ õàðàêòåðèñòèê öåíòðàëüíî-òèõîîêåàíñêîãî è âîñòî÷íî-òèõîîêåàíñêîãî Ýëü-Íèíüî â óñëîâèÿõ ïîòåïëåíèÿ êëèìàòà (ïî ðåçóëüòàòàì ýêñïåðèìåíòîâ RCP 2.6 è RCP 8.5 ïðîåêòà CMIP5)

Îöåíêà ÷àñòîòû è ñîîòíîøåíèÿ äâóõ òèïîâ Ýëü-Íèíüî, èíòåíñèâíîñòè è ðàñïðåäåëåíèÿ àíîìàëèé â îêåàíå è àòìîñôåðå ïðè ïîòåïëåíèè êëèìàòà. Õàðàêòåðèñòèêà êîëåáàíèÿ òåìïåðàòóðû ïîâåðõíîñòíîãî ñëîÿ âîäû â Òèõîì îêåàíå ïðè ðàçëè÷íûõ ñöåíàðèÿõ ïîòåïëåíèÿ.

Ðóáðèêà Áèîëîãèÿ è åñòåñòâîçíàíèå
Âèä ñòàòüÿ
ßçûê ðóññêèé
Äàòà äîáàâëåíèÿ 25.10.2018
Ðàçìåð ôàéëà 1,9 M

Îòïðàâèòü ñâîþ õîðîøóþ ðàáîòó â áàçó çíàíèé ïðîñòî. Èñïîëüçóéòå ôîðìó, ðàñïîëîæåííóþ íèæå

Ñòóäåíòû, àñïèðàíòû, ìîëîäûå ó÷åíûå, èñïîëüçóþùèå áàçó çíàíèé â ñâîåé ó÷åáå è ðàáîòå, áóäóò âàì î÷åíü áëàãîäàðíû.

Ïðîâåäåíî èññëåäîâàíèå âëèÿíèÿ èíòåíñèâíîñòè ðàäèàöèîííîãî ôîðñèíãà íà õàðàêòåðèñòèêè Ýëü-Íèíüî è íà ñîîòíîøåíèå ìåæäó êîëè÷åñòâîì äâóõ òèïîâ Ýëü-Íèíüî. Îòêëèê àíîìàëèé, ñâÿçàííûõ ñ äâóìÿ òèïàìè Ýëü-Íèíüî, íà óñèëåíèå ðàäèàöèîííîãî ôîðñèíãà ðàçëè÷åí - àíîìàëèè, ñâÿçàííûå ñ ÖÒ Ýëü-Íèíüî, óñèëèâàþòñÿ â îòâåò íà óâåëè÷åíèå ãëîáàëüíîãî ïîòåïëåíèÿ, èíòåíñèâíîñòü àíîìàëèé ïðè ÂÒ Ýëü-Íèíüî íå èìååò ÿðêî âûðàæåííîé çàâèñèìîñòè îò èçìåíåíèÿ ðàäèàöèîííîãî ôîðñèíãà. Ïîêàçàíî, ÷òî ñîîòíîøåíèå ìåæäó êîëè÷åñòâîì ñëó÷àåâ ÂÒ Ýëü-Íèíüî è ÖÒ Ýëü-Íèíüî çàâèñèò îò èíòåíñèâíîñòè ðàäèàöèîííîãî ôîðñèíãà: ïî íàèáîëåå "ñëàáîìó" ñöåíàðèþ (RCP 2.6) äîëÿ ÖÒ Ýëü-Íèíüî â îáùåì êîëè÷åñòâå ñëó÷àåâ Ýëü-Íèíüî ñîêðàùàåòñÿ, à ïðè íàèáîëåå èíòåíñèâíîì ïîòåïëåíèè (RCP 8.5) - âîçðàñòàåò.

Ïî ðåçóëüòàòàì äàííîãî èññëåäîâàíèÿ ìîæíî ñäåëàòü âûâîä î áîëüøîì ðàçáðîñå ìîäåëüíûõ îöåíîê èçìåíåíèÿ äâóõ òèïîâ Ýëü-Íèíüî â óñëîâèÿõ ïîòåïëåíèÿ êëèìàòà XXI âåêà. Îäíèì èç ïóòåé ðåøåíèÿ ïðîáëåìû íåîïðåäåë¸ííîñòè îöåíîê ìîæåò áûòü èñïîëüçîâàíèå äàííûõ ýêñïåðèìåíòîâ äëÿ áîëåå ò¸ïëûõ êëèìàòîâ ïðîøëîãî (Schmidtetal., 2014). Ìîäåëè, êîòîðûå èìåþò ðåàëèçàöèè â ïàëåîêëèìàòè÷åñêèõ ýêñïåðèìåíòàõ, ïðîõîäÿò âåðèôèêàöèþ íà ïàëåîäàííûõ, â òî âðåìÿ êàê îñóùåñòâèòü âåðèôèêàöèþ ýêñïåðèìåíòîâ ò¸ïëîãî êëèìàòà XXI âåêà íà äàííûõ íàáëþäåíèé íåâîçìîæíî. Òàêèì îáðàçîì, "ëó÷øèå" â âîñïðîèçâåäåíèè ïàëåîêëèìàòà ìîäåëè ìîãóò äàòü áîëåå íàä¸æíûå îöåíêè õàðàêòåðà èçìåíåíèÿ Ýëü-Íèíüî (ïåðèîäè÷íîñòè, àìïëèòóäû) â îòâåò íà ïîòåïëåíèå êëèìàòà, è òàêèì îáðàçîì áîëåå íàäåæíî îïðåäåëèòü âåêòîð èçìåíåíèé õàðàêòåðèñòèê Ýëü-Íèíüî â ò¸ïëîì êëèìàòå áóäóùåãî.

Áëàãîäàðíîñòè. Èññëåäîâàíèå áûëî âûïîëíåíî ïðè ôèíàíñîâîé ïîääåðæêå ÐÔÔÈ â ðàìêàõ ïðîåêòîâ ¹16-35-00394, ¹15-05-06693, ãîñáþäæåòíîé òåìû ¹ÀÀÀÀ-À 16-116032810086-4.

Ñïèñîê ëèòåðàòóðû

1. Æåëåçíîâà È.Â., Ãóùèíà Ä.Þ. 2016. Àíîìàëèè öèðêóëÿöèè â öåíòðàõ äåéñòâèÿ àòìîñôåðû â ïåðèîä Âîñòî÷íî-Òèõîîêåàíñêîãî è Öåíòðàëüíî-Òèõîîêåàíñêîãî Ýëü-Íèíüî. - Ìåòåîðîëîãèÿ è ãèäðîëîãèÿ, ¹ 11, c. 41-55.

2. Æåëåçíîâà È.Â., Ãóùèíà Ä.Þ. 2015. Îòêëèê ãëîáàëüíîé öèðêóëÿöèè àòìîñôåðû íà äâà òèïà Ýëü-Íèíüî. - Ìåòåîðîëîãèÿ è ãèäðîëîãèÿ, ¹ 3, ñ. 36-50.

3. Ïåòðîñÿíö Ì.À., Ñåìåíîâ Å.Ê., Ãóùèíà Ä.Þ., Ñîêîëèõèíà Å.Â., Ñîêîëèõèíà Í.Í. Öèðêóëÿöèÿ àòìîñôåðû â òðîïèêàõ. Êëèìàòèèçìåí÷èâîñòü, Ì.: ÌàêñÏðåññ, 2005, 560 ñ.

4. AnS. I. etal. Successive modulation of ENSO to the future greenhouse warming. 2008. - Journal of Climate, vol. 21 (1), p. 3-21.

5. AshokK. etal. 2007. El Niño Modoki and its possible teleconnection. - Journal of Geophysical Research: Oceans, vol. 112 (11), p. 1-27.

6. Bellenger H.et al. 2014. ENSO representation in climate models: from CMIP3 to CMIP5. - Climate Dynamics, vol. 42 (7-8), p. 1999-2018.

7. Bjerknes J. 1969. Atmospheric teleconnections from the equatorial Pacific. - Mon. Wea. Rev., vol. 97, pp.163-172.

8. Cai W. et al. 2014. Increasing frequency of extreme El Niño events due to greenhouse warming. - Nature climate change, vol. 4 (2), p. 111-116.

9. Cai W. et al. 2015.ENSO and greenhouse warming. - Nature Climate Change, vol. 5 (9), p. 849-859.

10. Capotondi A., Wittenberg A., Masina S. 2013.ENSO diversity in climate models. - US CLIVAR Variations, vol. 11 (2), p. 10-14.

11. Choi J. et al. 2011. The role of mean state on changes in El Nino's flavor. - Climate Dynamics, vol. 37 (5-6), p. 1205-1215.

12. Collins M. et al. 2010.The impact of global warming on the tropical Pacific Ocean and El Niño. - Nature Geoscience, vol. 3 (6), p. 391-397.

13. Cravatte S. et al. 2009. Observed freshening and warming of the western Pacific warm pool. - Climate Dynamics, vol. 33 (4), p. 565-589.

14. Definition of El Nin˜o and associated seasonal average U.S.

15. Definition of El Nin˜o and associated seasonal average U.S.

16. DiNezio P.N. et al. 2012. Climate Response of the Equatorial Pacific to Global Warming. - Journal of Climate, vol. 22 (18), p. 4873-4892.

17. doi:10.1029/2005GL022738.

18. doi:10.1029/2005GL022738.

19. Fedorov A.V. et al. 2013. Patterns and mechanisms of early Pliocene warmth. - Nature, vol. 496 (7443), p. 43-49.

20. Fedorov A.V., Philander S.G. 2000. Is El Niño changing? - Science, vol. 288(5473), p. 1997-2002.

21. Fedorov A.V. et al. 2006.The Pliocene paradox (mechanisms for a permanent El Nino). - Science, vol. 312, p. 1485-1489.

22. Ham Y.G., Jeong Y., Kug J.S. 2015. Changes in Independency between Two Types of El Niño Events under a Greenhouse Warming Scenario in CMIP5 Models. - Journal of Climate, vol.28 (19), p. 7561-7575.

23. Huber M. 2008.A Hotter Greenhouse? - Science, vol. 321, p. 353-354, doi: 10.1126/science.1161170.

24. Huber M. and R. Caballero. 2003. Eocene El Niño: Evidence for robust tropical dynamics in the "hothouse". - Science, vol. 299, p. 877-881.

25. Huffman G.J, R.F. Adler D.T. Bolvin G.Gu. 2009. Improving the Global Precipitation Record: GPCP Version 2.1. - Geophys. Res. Lett., vol. 36, L17808, doi:10.1029/2009GL040000.

26. Jian R., Rong-Cai R. 2014. Statistical characteristics of ENSO events in CMIP5 models. 2014. - Atmospheric and Oceanic Science Letters, vol. 7 (6), p. 546-552.

27. Jin F.F., An S.I. 1999. Thermocline and zonal advective feedbacks within the equatorial ocean recharge oscillator model for ENSO. - Geophysical research letters, vol. 26 (19), p. 2989-2992.

28. Johnson N.C. 2013. How many ENSO flavors can we distinguish? - Journal of Climate, vol. 26 (13), p. 4816-4827. doi:10.1175/JCLI-D-12-00649.1

29. Johnson N.C. 2014. Atmospheric science: A boost in big El Niño. - Nature Climate Change, vol. 4 (2), p. 90-91.

30. Kalnay E. and Co-authors. 1996. The NCEP/NCAR 40-year reanalysis project. - Bull. Amer. Meteor. Soc., vol. 77, p. 437-471.

31. Kao H.Y., Yu J.Y. 2009. Contrasting eastern-Pacific and central-Pacific types of ENSO. - Journal of Climate, vol. 22(3), p. 615-632, doi: 10.1175/2008JCLI2309.1

32. Kim S.T., Yu J.Y. 2012. The two types of ENSO in CMIP5 models. - Geophys. Res. Lett, vol.39, L11704,doi:10.1029/2012GL052006.

33. Kug J.S., Choi J., An S.I., Jin F.F., & Wittenberg A.T. 2010. Warm pool and cold tongue El Niño events as simulated by the GFDL 2.1 coupled GCM. - Journal of Climate, Vol. 23(5), p. 1226-1239. doi: 10.1175/2009JCLI3293.1

34. L'Heureux M. L., Lee S., Lyon B. 2013.Recent multidecadal strengthening of the Walker circulation across the tropical Pacific. - Nature Climate Change, vol. 3 (6),p. 571-576.

35. Larkin N.K., and Harrison D.E. 2005. On the definition of El Niño and associated seasonal average U.S. weather anomalies. - Geophys. Res. Lett., vol. 32, L13705, doi:10.1029/2005GL022738.

36. Latif M., Semenov V.A., Park W. 2015. Super El Niños in response to global warming in a climate model. - Climatic Change, vol. 132 (4), p. 489-500.

37. Lee T., McPhaden M.J. 2010. Increasing intensity of El Niño in the central?equatorial Pacific. - Geophysical Research Letters, vol. 37 (14), p. L14603.

38. Lengaigne M., Vecchi G.A. 2010. Contrasting the termination of moderate and extreme El Niño events in coupled general circulation models. - Climate dynamics, vol. 35 (2-3), p. 299-313.

39. McPhaden M.J., Lee T., McClurg D. 2011. El Niño and its relationship to changing background conditions in the tropical Pacific Ocean. - Geophysical Research Letters, vol. 38 (15), p. L15709.

40. Medhaug I., Drange H. 2016. Global and regional surface cooling in a warming climate: a multi-model analysis. - Climate Dynamics,vol. 46 (11-12), p. 3899-3920.

41. Meng Q. et al. 2012. Twentieth century Walker Circulation change: Data analysis and model experiments. - Climate dynamics, vol. 38 (9-10), p. 1757-1773.

42. Power S. et al. 2013. Robust twenty-first-century projections of El Niño and related precipitation variability. - Nature, vol. 502 (7472), p. 541-545.

43. Rayner N. A et al. 2003. Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. - J. Geophys. Res., 2003, vol. 108(D14), pp. 4407, doi:10.1029/ 2002JD002670.

44. Rogelj J., MeinshausenM., KnuttiR. 2012. Global warming under old and new scenarios using IPCC climate sensitivity range estimates. - Nature climate change, vol. 2 (4), p. 248-253.

45. Santoso A. et al. 2013. Late-twentieth-century emergence of the El Niño propagation asymmetry and future projections. - Nature, vol. 504 (7478), p. 126-130.

46. Sen Gupta A. et al. 2012. Drivers of the projected changes to the Pacific Ocean equatorial circulation. - Geophysical Research Letters, vol. 39 (9), p. L09605.

47. Schmidt G.A. et al. (2014).Using paleo-climate comparisons to constrain future projections in CMIP5.ClimateofthePast, 10(1), 221-250.

48. Taschetto A. S et al. 2014. Cold tongue and warm pool ENSO events in CMIP5: Mean state and future projections. - Journal of Climate, vol. 27 (8), p. 2861-2885, doi:10.1175/ JCLI-D-13-00437.1.

49. Taylor K.E., Stouffer R.J., Meehl G.A. 2012. An overview of CMIP5 and the experiment design. - Bulletin of the American Meteorological Society, vol. 93 (4), p. 485-498.

50. Trenberth K.E., Hoar T.J. 1996. The 1990-1995 El Niño?Southern Oscillation event: Longest on record. - Geophysical Research Letters, vol. 23 (1), p. 57-60.

51. Van Vuuren, D. P et al. 2011. The representative concentration pathways: an overview. - Climatic change, vol. 109, p. 5-31.

52. Vecchi G.A., Soden B.J. 2007. Global warming and the weakening of the tropical circulation. - Journal of Climate, vol. 20 (17), p. 4316-4340.

53. Wang D. et al. 2015. Intensification and spatial homogenization of coastal upwelling under climate change. - Nature, vol. 518 (7539), p. 390-394.

54. Weather anomalies, Geophys. Res. Lett., 32, L13705.

55. Weng H., Behera S.K. and Yamagata T. 2009. Anomalous winter climate conditions in the Pacific Rim during recent El Nino Modoki and El Nino events. - Clim. Dyn., vol. 32, p. 663-674.

56. Wunsch C. 2009. A perpetually running ENSO in the Pliocene? - Journal of Climate, vol. 22 (12), p. 3506-3510.

57. Xiang B. et al. 2014. Understanding the anthropogenically forced change of equatorial Pacific trade winds in coupled climate models. - Journal of Climate, vol. 27 (22), p. 8510-8526.

58. Xie S.P. et al. 2010. Global warming pattern formation: sea surface temperature and rainfall. - Journal of Climate, vol. 23 (4), p. 966-986.

59. Xu K. et al. 2017. CMIP5 Projections of Two Types of El Niño and Their Related Tropical Precipitation in the Twenty-First Century. - Journal of Climate, vol. 30 (3), p. 849-864.

60. Yeh S. -W.et al.2009. El Niño in a changing climate. - Nature, vol. 461, p. 511-514.

61. Zhang T., Sun D.Z. 2014.ENSO asymmetry in CMIP5 models. - Journal of Climate,vol. 27 (11), p. 4070-4093.

Ðàçìåùåíî íà Allbest.ru

...

Ïîäîáíûå äîêóìåíòû

  • Îïðåäåëåíèå ïîíÿòèÿ áèîãåîöåíîçà â îêåàíå. Ôëîðà è ôàóíà ïîâåðõíîñòíîé ïëåíêè âîäû è çîíû çîîïëàíêòîíà. Ðàñòèòåëüíî-æèâîòíûå ñîîáùåñòâà çîíû ôèòîçîîãåîöåíîçîâ. Êîñíûå, áèîêîñíûå è áèîëîãè÷åñêèå ôàêòîðû ðåãóëèðîâàíèÿ ôîðìèðîâàíèÿ ìîðñêèõ áèîãåîöåíîçîâ.

    ïðåçåíòàöèÿ [357,4 K], äîáàâëåí 28.02.2014

  • Ðàçíîîáðàçèå æèçíè â îêåàíå: îáèòàòåëè ïîäâîäíîãî ìèðà. ßðêàÿ îêðàñêà è íåîáû÷íûå çóáû ðûáû-ïîïóãàÿ, åå ñïîñîá çàùèòû. Ñàìîå áîëüøîå æèâîòíîå – êèò. Ìîðñêèå àêðîáàòû – ìîðñêèå ñâèíüè è äåëüôèíû. Ñàìàÿ ñòðàøíàÿ ðûáà – àêóëà. Ìîðñêèå çâåçäû, èëèñòûé ïðûãóí.

    ïðåçåíòàöèÿ [2,6 M], äîáàâëåí 17.05.2012

  • Õàðàêòåðèñòèêà æèçíåäåÿòåëüíîñòè áàðåíöåâîìîðñêèõ ìèäèé. Ôàêòîðû ñðåäû è ðàçìíîæåíèå. Ïðèðîäíîå èíèöèèðîâàíèå âûìåòà ïîä âîçäåéñòâèåì ïîòåïëåíèÿ. Ìèäèè êàê ïåðñïåêòèâíûé îáúåêò àêâàêóëüòóðû. Ìåòîäèêà ýêñïåðèìåíòîâ ïî ðåãèñòðàöèè äâèãàòåëüíîé àêòèâíîñòè.

    êóðñîâàÿ ðàáîòà [793,0 K], äîáàâëåí 09.12.2013

  • Ñóùíîñòü ãëîáàëüíîãî ïîòåïëåíèÿ. Ãèïîòåçû è ïðåäïîëîæåíèÿ î åãî ïðè÷èíàõ. Èíñòðóìåíòû, ïðèìåíÿåìûå ó÷åíûìè äëÿ èçó÷åíèÿ êëèìàòè÷åñêèõ èçìåíåíèé. Ôàêòîðû, âëèÿþùèå íà êëèìàò ïëàíåòû. Ïîñëåäñòâèÿ óâåëè÷åíèÿ òåìïåðàòóðû àòìîñôåðû. Ñïîñîáû åãî ïðåäîòâðàùåíèÿ.

    ïðåçåíòàöèÿ [1,4 M], äîáàâëåí 05.11.2014

  • Öóíàìè — äëèííûå âîëíû, ïîðîæäàåìûå ìîùíûì âîçäåéñòâèåì íà âñþ òîëùó âîäû â îêåàíå. Ïðè÷èíû îáðàçîâàíèÿ öóíàìè: ïîäâîäíûå çåìëåòðÿñåíèÿ, ñìåùåíèå ó÷àñòêà ìîðñêîãî äíà. Ïðèçíàêè ïîÿâëåíèÿ öóíàìè, èõ îïàñíîñòü, ïðàâèëà ïîâåäåíèÿ; ñèñòåìû ïðåäóïðåæäåíèÿ.

    ïðåçåíòàöèÿ [1,5 M], äîáàâëåí 28.10.2013

  • Êàòàñòðîôè÷åñêèå ïðèðîäíûå ÿâëåíèÿ. Öóíàìè - äëèííûå âîëíû, ïîðîæäàåìûå ìîùíûì âîçäåéñòâèåì íà âñþ òîëùó âîäû â îêåàíå, ïðè÷èíû èõ îáðàçîâàíèÿ, ðàçðóøèòåëüíûå ïîñëåäñòâèÿ. Ïðèçíàêè ïðèáëèæåíèÿ öóíàìè, ïðàâèëà áåçîïàñíîñòè, ñèñòåìû ïðåäóïðåæäåíèÿ.

    ïðåçåíòàöèÿ [368,1 K], äîáàâëåí 17.03.2014

  • Ïîíÿòèå î ãèäðîñôåðå è ëèòîñôåðå. Àòìîñôåðà êàê âîçäóøíàÿ îáîëî÷êà ïëàíåòû, å¸ ñîñòàâ. Âíóòðåííåå ñòðîåíèå Çåìëè. Ðàñïðåäåëåíèå âîäû â ãèäðîñôåðå. Ðîëü îçîíîâîãî ñëîÿ â àòìîñôåðå. Ãðóíòîâûå è ïîäçåìíûå âîäû. Áèîñôåðà êàê îáëàñòü ðàñïðîñòðàíåíèÿ æèçíè.

    ïðåçåíòàöèÿ [2,7 M], äîáàâëåí 18.10.2015

  • Äûõàíèå êàê ôèçèîëîãè÷åñêèé ïðîöåññ, îáåñïå÷èâàþùèé íîðìàëüíûé ìåòàáîëèçì æèâûõ îðãàíèçìîâ. Îñîáåííîñòè äûõàíèÿ â èçìåíåííûõ óñëîâèÿõ. Âëèÿíèå íà ïðîöåññ äûõàíèÿ æàðêîãî êëèìàòà. Äûõàíèå â óñëîâèÿõ âûñîêîãîðüÿ è ïîâûøåííîãî áàðîìåòðè÷åñêîãî äàâëåíèÿ.

    ïðåçåíòàöèÿ [627,4 K], äîáàâëåí 03.12.2015

  • Îñîáåííîñòè ïðîèñõîäèâøèõ íà çàðå èñòîðèè ïëàíåòû Çåìëÿ êëèìàòè÷åñêèõ òðàíñôîðìàöèé. Òåìïåðàòóðíûå êîëåáàíèÿ àòìîñôåðû è âîä, èçìåíåíèå êîíôèãóðàöèè êîíòèíåíòîâ â äðåâíèå âðåìåíà. Ôàêòîðû îáëåäåíåíèÿ ïîëþñîâ. Èçìåíåíèå êëèìàòà â ×åòâåðòè÷íûé ïåðèîä.

    ñòàòüÿ [12,9 K], äîáàâëåí 27.12.2009

  • Ìåñòà îáèòàíèÿ êèòîâûõ îëóøåé. Ïîõîëîäàíèå - ïðèçíàê èçìåíåíèÿ êëèìàòà â ïåðèîä îáëåäåíåíèÿ, åãî ïîñëåäñòâèÿ. Æèçíåííûå óñëîâèÿ ñêðîô, ÿùåðèö, êàðàêàð è ñïèíîãðîìà. Èçìåíåíèÿ â ïîâåäåíèè è ñòðîåíèè òåëà áàáóêàðè ïðè ñóùåñòâîâàíèè íà îòêðûòîì ïðîñòðàíñòâå.

    ðåôåðàò [2,0 M], äîáàâëåí 13.11.2012

  • Âëèÿíèå êëèìàòà è ïèòàíèÿ íà ðàçíèöó â öâåòå êîæè, òåëîñëîæåíèè, ðàçìåðàõ ÷åëþñòåé æèòåëåé ðàçíûõ ìàòåðèêîâ. Óçêèé ðàçðåç ãëàç ó êîðåííûõ íàðîäîâ Ñåâåðà êàê ñëåäñòâèå îñëåïëåíèÿ îòðàæåííûìè îò ñíåãà ëó÷àìè ñîëíöà. Âëèÿíèå èçìåíåíèÿ ìåñòà ïðîæèâàíèÿ.

    ðåôåðàò [11,4 K], äîáàâëåí 18.01.2010

  • Îñîáåííîñòè êëèìàòà â äîêåìáðèéñêîì, ïàëåîçîéñêîì è ìåçîçîéñêîì ïåðèîäàõ. Ïðè÷èíû ìàëîãî êëèìàòè÷åñêîãî îïòèìóìà Ñðåäíåâåêîâüÿ. Ôàçû ìàëîãî ëåäíèêîâîãî ïåðèîäà, åãî ïðè÷èíû. Âëèÿíèå êëèìàòà íà ïðîèçâîäñòâî, ðàñïðåäåëåíèå âîäíûõ è ýíåðãåòè÷åñêèõ ðåñóðñîâ.

    ðåôåðàò [34,4 K], äîáàâëåí 24.05.2015

  • Èçìåíåíèÿ òåìïåðàòóðû âîäû â óñëîâèÿõ ñîâðåìåííîãî èíòåíñèâíîãî ãèäðîñòðîèòåëüñòâà êàê ôàêòîð, âëèÿþùèé íà æèçíü ãèäðîáèîíòîâ. Áèîëîãè÷åñêèå õàðàêòåðèñòèêè ìàññîâûõ âèäîâ-àêêëèìàòèçàíòîâ, ïðè÷èíû ãèáåëè òðîïè÷åñêîé èõòèîôàóíû â Êàðàñóíñêèõ îçåðàõ.

    äèïëîìíàÿ ðàáîòà [2,7 M], äîáàâëåí 30.12.2014

  • Õàðàêòåðèñòèêà è êëàññèôèêàöèÿ ìîëëþñêîâ. Îáùèé ïëàí èõ ñòðîåíèÿ. Ðîëü ìîëëþñêîâ â Ìèðîâîì îêåàíå è â æèçíè ÷åëîâåêà. Èñïîëüçîâàíèå â ñîâðåìåííîé ïðîìûøëåííîñòè ðàêîâèíû ðå÷íîé ïåðëîâèöû. Âðåäíîå çíà÷åíèå ñëèçíÿêà. Ìåäèöèíñêîå çíà÷åíèå ìîëëþñêîâ.

    êóðñîâàÿ ðàáîòà [265,1 K], äîáàâëåí 24.04.2017

  • Ïîíÿòèå è ñòðóêòóðà Ñîëíå÷íîé ñèñòåìû. Õàðàêòåðèñòèêà è ñóùíîñòü çàêîíà âñåìèðíîãî òÿãîòåíèÿ. Îïèñàíèå ñàìûõ ãëàâíûõ õèìè÷åñêèõ ýëåìåíòîâ äëÿ æèçíè: ìàãíèé, óãëåðîä, êèñëîðîä, ìàðãàíåö. Àíàëèç îñíîâíûõ ïðè÷èí ãëîáàëüíîãî èçìåíåíèÿ êëèìàòà íà Çåìëå.

    êîíòðîëüíàÿ ðàáîòà [220,7 K], äîáàâëåí 26.04.2012

  • Ðàñòåíèÿ, îáëàäàþùèå ëåêàðñòâåííûìè ñâîéñòâàìè. Ïðèìåíåíèå ëåêàðñòâåííûõ ðàñòåíèé â ìåäèöèíå, âåòåðèíàðèè è ïèùåâîé ïðîìûøëåííîñòè. Ñâîéñòâà àäîíèñà àìóðñêîãî, àèðà îáûêíîâåííîãî, áàäàíà òèõîîêåàíñêîãî, âèíîãðàäà àìóðñêîãî è äåâÿñèëà ÿïîíñêîãî.

    ïðåçåíòàöèÿ [328,4 K], äîáàâëåí 18.11.2014

  • Ïðèíöèïû ïåðåäà÷è íàñëåäñòâåííûõ ïðèçíàêîâ îò ðîäèòåëüñêèõ îðãàíèçìîâ ê èõ ïîòîìêàì, âûòåêàþùèå èç ýêñïåðèìåíòîâ Ãðåãîðà Ìåíäåëÿ. Ñêðåùèâàíèå äâóõ ãåíåòè÷åñêè ðàçëè÷íûõ îðãàíèçìîâ. Íàñëåäñòâåííîñòü è èçìåí÷èâîñòü, èõ âèäû. Ïîíÿòèå î íîðìå ðåàêöèè.

    ðåôåðàò [19,2 K], äîáàâëåí 22.07.2015

  • Æèçíåííûé öèêë êàøàëîòà. Ïðèíöèïû äåéñòâèÿ ãèäðîëîêàòîðîâ êèòà. Îðèåíòèðîâêà íà ìåñòíîñòè â ãëóáèíå îêåàíà. Ðàçíîîáðàçèå æèçíè â ãëóáèíå. Ôîðìû æèçíè íà Ãàëàïàãîññêèõ îñòðîâàõ. Âîäíûå òå÷åíèÿ ó Àìåðèêàíñêîãî êîíòèíåíòà. Ýôôåêòû ãëîáàëüíîãî ïîòåïëåíèÿ.

    ðåôåðàò [31,1 K], äîáàâëåí 05.11.2012

  • Îáùèå ñâåäåíèÿ î áåëûõ ìåäâåäÿõ: âíåøíèé âèä, ðàñïðîñòðàíåíèå, îáðàç æèçíè è ïèòàíèå. Îñîáåííîñòè èõ ñîöèàëüíîé ñòðóêòóðû è ðàçìíîæåíèÿ. Âëèÿíèå ãëîáàëüíîãî ïîòåïëåíèÿ íà ïîïóëÿöèþ áåëûõ ìåäâåäåé. Çàâèñèìîñòü ðîñòà ÷èñëåííîñòè ïîïóëÿöèè îò ðîæäàåìîñòè.

    êóðñîâàÿ ðàáîòà [2,6 M], äîáàâëåí 20.09.2012

  • ×òî òàêîå îïóñòûíèâàíèå. Ïîñòåïåííîå ïðåâðàùåíèå çàñóøëèâûõ çåìåëü â ïóñòûíþ. Ïîñëåäñòâèÿ îïóñòûíèâàíèÿ â ýêîëîãè÷åñêîì è ýêîíîìè÷åñêîì îòíîøåíèè. Äåôèöèò âîäû, àðèäèçàöèÿ êëèìàòà, âûðóáêà ëåñà, ïåðåïàñ ñêîòà, áèîëîãè÷åñêàÿ ãèáåëü, ïîòåðè ïëîäîðîäèÿ.

    ðåôåðàò [87,4 K], äîáàâëåí 09.05.2011

Ðàáîòû â àðõèâàõ êðàñèâî îôîðìëåíû ñîãëàñíî òðåáîâàíèÿì ÂÓÇîâ è ñîäåðæàò ðèñóíêè, äèàãðàììû, ôîðìóëû è ò.ä.
PPT, PPTX è PDF-ôàéëû ïðåäñòàâëåíû òîëüêî â àðõèâàõ.
Ðåêîìåíäóåì ñêà÷àòü ðàáîòó.