this is an example answer questions 3 and 4 using the examples above Example- yo

Question

this is an example

answer questions 3 and 4 using the examples above

Example- yours should look like this Non-Human Organisms Coral, climate vegetation- plants, trees, ocean creatures- corals squid, polar bears, microorganisms- bacteria, fungi, viruses Citation lhamsyah, Yopi; Fadli, Nur; Setiawan, Ichsan; Haridhi, Haekal A. Aquaculture, Aquarium, Conservation & Legislation - International Journal of the Bioflux Society (AACL Bioflux). 2014, Vol. 7 Issue 6, p508- 515. 8p The author's intention was to study coral bleaching near Wey Island in Indonesia. The purpose of the study was to determine if El Nino southern oscillation and Indian ocean Dipole, which are naturally occurring, are the cause of coral bleaching for the time period they researched. The researchers found that coral biodiversity decreases in the time preceding El Nino and Indian Ocean Dipole. Summary

Explanation / Answer

Land or Ocean

Glaciation, Oxygen Isotope, Sea-level changes

Citation

Aharon, P., Chappell, J., Compston, W., Stable isotope and sea-level data from New Guinea supports Antarctic ice-surge theory of ice ages, Nature 283, 649–651,1980,doi:10.1038/283649a0

Summary

Glaciation over past geologic time has two theory- one is Milankovitch orbital theory where a change in the orbital parameter is considered and another is the Antarctic surge hypothesis where the Earth's albedo increased due to a surge of Antarctic ice sheet in the southern ocean. The last interglacial maximum at 125 kyr and then decline with cooling of the North Atlantic, and with cooling of the North Atlantic that triggered a succeeding ice age. The raised coral reefs of Huon Peninsula, Papua New Guinea, contain a particularly good record of the interval 140–105 kyr which providing oxygen isotope and sea-level data that seem to require an Antarctic surge at 120 kyr, and which also have a role of the Milankovitch factor in it.

Atmosphere

Urban rainfall, atmospheric boundary layer

Citation

Collier, C. G., The impact of urban areas on weather, Q. J. R. Meteorol. Soc. (2006), 132, pp. 1–25, doi: 10.1256/qj.05.199

Summary

Planetary boundary layer over an urban area is heterogeneous and has an implication of energy budget, water budget, and weather phenomenon. This layer has the direct effect on human life and defined as the layer from canopy layer to bottom cloud surface. Doppler lidar which can measure above canopy layer properties has been used for the study of the urban atmospheric boundary layer, considering the impact of a high-rise building. In-situ surface based remote sensing, complex numerical analysis succeeded to show the balance between interaction such as urban heat island, convectional rainfall etc. The study found that the urban weather is 10° warmer than rural area, attracting the more precipitation over it. Limitation including aerosol’s negative effect needed to be further researched.

Land or Ocean

Glaciation, Oxygen Isotope, Sea-level changes

Citation

Aharon, P., Chappell, J., Compston, W., Stable isotope and sea-level data from New Guinea supports Antarctic ice-surge theory of ice ages, Nature 283, 649–651,1980,doi:10.1038/283649a0

Summary

Glaciation over past geologic time has two theory- one is Milankovitch orbital theory where a change in the orbital parameter is considered and another is the Antarctic surge hypothesis where the Earth's albedo increased due to a surge of Antarctic ice sheet in the southern ocean. The last interglacial maximum at 125 kyr and then decline with cooling of the North Atlantic, and with cooling of the North Atlantic that triggered a succeeding ice age. The raised coral reefs of Huon Peninsula, Papua New Guinea, contain a particularly good record of the interval 140–105 kyr which providing oxygen isotope and sea-level data that seem to require an Antarctic surge at 120 kyr, and which also have a role of the Milankovitch factor in it.

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