{'annex_type': 'Non-Annex I', 'IkiSheet': 'targets', 'page_number': nan, 'renewable_energy_target': nan, 'transport_target_type': nan, 'target_year': nan, 'country_netzero target_exists': nan, 'country_summary_transport_targets': nan, 'target_type': 'T_BYE', 'oecd': 'non-OECD', 'income_group': 'Middle-income', 'g7': 0, 'mena': 0, 'region': 'Latin America and the Caribbean', 'parameter': 'T_Economy_Unc', 'ice_phaseout': nan, 'country_long-term_target_exists': nan, 'ghg_total': 56.28605778513, 'ghg_transport_target_type': nan, 'g20': 0, 'target_scope': nan, 'ghg_transport': 23.135968263}
Climate scenarios predict water regime irregularities in 2030. In the Mountain regions, it is predicted that annual rainfalls would show deficiencies between -10% and -20%; in the northern and central Amazon area (high jungle) annual rainfalls it would be up to -10%, and in the northern and southern coast it
Climate scenarios predict water regime irregularities in 2030. In the Mountain regions, it is predicted that annual rainfalls would show deficiencies between -10% and -20%; in the northern and central Amazon area (high jungle) annual rainfalls it would be up to -10%, and in the northern and southern coast it would show increases between + 10% and + 20%.
20% below 2030 BAU