proposals – Addendum
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DETAILED PROJECT / PROGRAMME DESCRIPTION<br />
GREEN CLIMATE FUND FUNDING PROPOSAL | PAGE 12 OF 101<br />
C<br />
If intense droughts increase in frequency, as suggested by global climate models (Cox et al. 2004; Betts et al. 2004),<br />
large areas of the Amazon’s forest canopy would likely be exposed to the persistent effect of drought and the slow<br />
recovery of forest canopy structure and function. Early signs of potential large-scale degradation of the Amazon<br />
rainforest from climate change ,3 4 through increased rainfall variability in the past decade, may already be present in<br />
areas of the southern and western Amazon.<br />
Floods, and especially the combination of intense droughts and high floods, as has recently occurred (2012) in the<br />
Amazon Basin, have the potential for disrupting ecosystems, and could result in permanent changes in biodiversity and<br />
ecosystem services. Floods have produced severe damages to dwellings and infrastructure, have destroyed crops and<br />
killed domestic animals, have caused economic hardships, and are associated with severe outbreaks of diseases and ill<br />
health. Indigenous communities in the project area have observed flood stages never before reached, and have<br />
expressed their concern about the increased frequency of floods. These communities’ observations confirm conclusions<br />
reached by scientists through analyses using complex analytical tools.<br />
Infrastructure projects. The construction of large transportation infrastructure is also a major concern for the carbon<br />
stock in PDM. Several large projects are under consideration by the national and regional governments. The Loreto<br />
region lacks major roadways connecting it to the rest of the country. Its regional government has presented a<br />
transportation plan to the Ministry of Transportation and Public Works. This plan analyses the need for different modes<br />
of transportation and according to it, the first priority is a road connecting Iquitos to Yurimaguas. 5 The construction of<br />
this road is a long-held dream that is not viable in the near future. Loreto will eventually be connected to the rest of the<br />
country through the road system, and this is a likely option to start with. Whatever the GOP decides, the road will<br />
accelerate deforestation and increase land grabbing and land degradation. If not well managed, the road is likely to<br />
have a severe impact on the carbon stock in the project area.<br />
Threats to the population<br />
The processes described above are likely to impact the population living in the project area. Based on existing<br />
information, it is estimated that minimum temperatures are increasing, and are likely to continue increasing in the future.<br />
The Meteorological and Hydrological National Service of Peru (SENAMHI) suggests that they are likely to increase<br />
between 4.0 and 6.0 o C, while the estimated range of increments for average temperatures is between 3.6 and 5.2 °C.<br />
Heatwaves are also expected to become more frequent, with estimates of 2.28 additional hot nights per decade and 1.2<br />
additional very hot days per decade.<br />
Floods are likely to become more frequent, changing the character of the alluvial rivers, especially in their deposition<br />
cones in the Andean foothills. Climate models and scenarios of future climate conditions do not offer guidance about<br />
expected changes in the river channel. More frequent floods, as already experienced in the Amazon, are likely to have<br />
serious impacts on the well-being of the population, its health and transportation costs.<br />
Underlying causes of deforestation<br />
From the above discussion, from PROFONANPE experiences working in the area for the past eight years, from<br />
technical literature and from the REDD-plus initiatives in Peru, the main underlying causes of deforestation have been<br />
identified. Due to their particular relevance in Loreto and PDM, we highlight the following:<br />
3<br />
Zelazowski P, Malhi Y, Huntingford C, Sitch S, Fisher JB. 2011. Changes in the potential distribution of humid<br />
tropical forests on a warmer planet. Philos Transact A Math Phys Eng Sci 369(1934):137<strong>–</strong>160.<br />
4<br />
Saatchi S, Asefi-Najafabady M, Aragão LEOC, Anderson LO, Myneni RB, and Nemani R. 2013.“Persistent effects<br />
of a severe drought on Amazonian forest canopy. Proceedings of the National Academy of Sciences, available at<br />
.<br />
5<br />
See .